Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface

In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs. Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Zhang, Junli [verfasserIn] Kopf, Achim [akademischer betreuerIn] Behrmann, Jan Hinrich - 1953- [akademischer betreuerIn]
Körperschaften:	Universität Bremen [Grad-verleihende Institution]
Hochschulschrift:	Dissertation ; Universität Bremen ; 2021

Format:	E-Book
Sprache:	Englisch

Erschienen:	Bremen: 2021

Schlagwörter:	pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones
Formangabe:	Hochschulschrift

Umfang:	1 Online-Ressource (124 Seiten) ; Illustrationen

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Zhang, Junli: Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface - Bremen, 2021

Links:	Link aufrufen Link aufrufen Link aufrufen Link aufrufen Link aufrufen

DOI / URN:	urn:nbn:de:gbv:46-elib58150 10.26092/elib/1438

Katalog-ID:	1797019651

Internformat


LEADER	01000cam a2200265 4500
001	1797019651
003	DE-627
005	20240912025502.0
007	cr uuu---uuuuu
008	220330s2021 gw \|\|\|\|\|om 00\| \|\|eng c
024	7		\|a urn:nbn:de:gbv:46-elib58150 \|2 urn
024	7		\|a 10.26092/elib/1438 \|2 doi
035			\|a (DE-627)1797019651
035			\|a (DE-599)KXP1797019651
035			\|a (OCoLC)1311518074
040			\|a DE-627 \|b ger \|c DE-627 \|e rda
041			\|a eng
044			\|c XA-DE-HB
082	0	4	\|a 551.22 \|q DE-101
082	0	4	\|a 550 \|q DE-101
100	1		\|a Zhang, Junli \|e verfasserin \|0 (orcid)0000-0002-2546-8633 \|4 aut
245	1	0	\|a Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface \|c submitted by Junli Zhang
264		1	\|a Bremen \|c 2021
300			\|a 1 Online-Ressource (124 Seiten) \|b Illustrationen
336			\|a Text \|b txt \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
502			\|b Dissertation \|c Universität Bremen \|d 2021
520			\|a In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs.
583	1		\|a Archivierung/Langzeitarchivierung gewährleistet \|f PEHB \|x XA-DE-HB \|2 pdager \|5 DE-46
650		4	\|a pore pressure
650		4	\|a consolidation experiments
650		4	\|a tsunamigenic earthquakes
650		4	\|a slow slip events
650		4	\|a subduction zones
655		7	\|a Hochschulschrift \|0 (DE-588)4113937-9 \|0 (DE-627)105825778 \|0 (DE-576)209480580 \|2 gnd-content
700	1		\|a Kopf, Achim \|e akademischer betreuerin \|0 (DE-588)1057165131 \|0 (DE-627)795691181 \|0 (DE-576)413695298 \|4 dgs
700	1		\|a Behrmann, Jan Hinrich \|d 1953- \|e akademischer betreuerin \|0 (DE-588)143664867 \|0 (DE-627)653840470 \|0 (DE-576)338247793 \|4 dgs
710	2		\|a Universität Bremen \|e Grad-verleihende Institution \|0 (DE-588)2001386-3 \|0 (DE-627)101380429 \|0 (DE-576)191575038 \|4 dgg
751			\|a Bremen \|0 (DE-588)4008135-7 \|0 (DE-627)106369636 \|0 (DE-576)208874569 \|4 uvp
776	0	8	\|i Erscheint auch als \|n Druck-Ausgabe \|a Zhang, Junli \|t Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface \|d Bremen, 2021 \|h 124 Seiten \|w (DE-627)1797019996
856	4	0	\|u http://dx.doi.org/10.26092/elib/1438 \|x Resolving-System \|z kostenfrei
856	4	0	\|u https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 \|x Resolving-System \|z kostenfrei
856	4	0	\|u https://d-nb.info/1338948229/34 \|x Langzeitarchivierung Nationalbibliothek \|z kostenfrei
856	4	0	\|u https://media.suub.uni-bremen.de/handle/elib/5815 \|x Verlag \|z kostenfrei
912			\|a GBV-ODiss
912			\|a GBV_ILN_20
912			\|a ISIL_DE-84
912			\|a SYSFLAG_1
912			\|a GBV_KXP
912			\|a GBV_ILN_21
912			\|a ISIL_DE-46
912			\|a GBV_ILN_22
912			\|a ISIL_DE-18
912			\|a GBV_ILN_23
912			\|a ISIL_DE-830
912			\|a GBV_ILN_30
912			\|a ISIL_DE-104
912			\|a GBV_ILN_40
912			\|a ISIL_DE-7
912			\|a GBV_ILN_60
912			\|a ISIL_DE-705
912			\|a GBV_ILN_63
912			\|a ISIL_DE-Wim2
912			\|a GBV_ILN_70
912			\|a ISIL_DE-89
912			\|a GBV_ILN_105
912			\|a ISIL_DE-841
912			\|a GBV_ILN_110
912			\|a ISIL_DE-Luen4
912			\|a GBV_ILN_132
912			\|a ISIL_DE-959
912			\|a GBV_ILN_151
912			\|a ISIL_DE-546
912			\|a GBV_ILN_161
912			\|a ISIL_DE-960
912			\|a GBV_ILN_293
912			\|a ISIL_DE-960-3
912			\|a GBV_ILN_370
912			\|a ISIL_DE-1373
912			\|a GBV_ILN_2403
912			\|a ISIL_DE-LFER
935			\|i DSpace
951			\|a BO
980			\|2 20 \|1 01 \|x 0084 \|b 4593077184 \|y x \|z 12-10-24
980			\|2 21 \|1 01 \|x 0046 \|b 4106904322 \|h ebook_2022_dissbremen \|k Kostenloser Zugriff \|y zza \|z 30-03-22
980			\|2 22 \|1 01 \|x 0018 \|b 4593180066 \|h SUBolrd \|y xu \|z 12-10-24
980			\|2 23 \|1 01 \|x 0830 \|b 459322912X \|h olr-d \|y x \|z 12-10-24
980			\|2 30 \|1 01 \|x 0104 \|b 4593276152 \|y z \|z 12-10-24
980			\|2 40 \|1 01 \|x 0007 \|b 4593309697 \|y xsn \|z 12-10-24
980			\|2 60 \|1 01 \|x 0705 \|b 4593367433 \|h OLRD \|y z \|z 12-10-24
980			\|2 63 \|1 01 \|x 3401 \|b 4593423171 \|h ORD \|y x \|z 12-10-24
980			\|2 70 \|1 01 \|x 0089 \|b 4593474175 \|y z \|z 12-10-24
980			\|2 105 \|1 01 \|x 0841 \|b 4593865778 \|y z \|z 12-10-24
980			\|2 110 \|1 01 \|x 3110 \|b 4593578078 \|y x \|z 12-10-24
980			\|2 132 \|1 01 \|x 0959 \|b 4593621836 \|h OLR-DISS \|y x \|z 12-10-24
980			\|2 151 \|1 01 \|x 0546 \|b 4593664993 \|h OLR-ODISS \|y z \|z 12-10-24
980			\|2 161 \|1 01 \|x 0960 \|b 4593688027 \|h ORD \|y z \|z 12-10-24
980			\|2 293 \|1 01 \|x 3293 \|b 4593815827 \|h ORD \|y z \|z 12-10-24
980			\|2 370 \|1 01 \|x 4370 \|b 4593853710 \|y x \|z 12-10-24
980			\|2 2403 \|1 01 \|x DE-LFER \|b 4113689865 \|c 00 \|f --%%-- \|d --%%-- \|e n \|j --%%-- \|y l01 \|z 08-04-22
981			\|2 20 \|1 01 \|x 0084 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 21 \|1 01 \|x 0046 \|r https://doi.org/10.26092/elib/1438 \|z LF
981			\|2 22 \|1 01 \|x 0018 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 23 \|1 01 \|x 0830 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 30 \|1 01 \|x 0104 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 40 \|1 01 \|x 0007 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 60 \|1 01 \|x 0705 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 63 \|1 01 \|x 3401 \|y E-Book \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 \|z LF
981			\|2 70 \|1 01 \|x 0089 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 105 \|1 01 \|x 0841 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 110 \|1 01 \|x 3110 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 132 \|1 01 \|x 0959 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 151 \|1 01 \|x 0546 \|y Volltext \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 161 \|1 01 \|x 0960 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 293 \|1 01 \|x 3293 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 370 \|1 01 \|x 4370 \|r https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150
981			\|2 2403 \|1 01 \|x DE-LFER \|r http://dx.doi.org/10.26092/elib/1438
982			\|2 21 \|1 00 \|x DE-46 \|8 00 \|a Universität Bremen
983			\|2 60 \|1 01 \|x 0705 \|8 10 \|a ho
985			\|2 20 \|1 01 \|x 0084 \|a OLRD
985			\|2 110 \|1 01 \|x 3110 \|a OLRD
985			\|2 370 \|1 01 \|x 4370 \|a OLRD
995			\|2 21 \|1 01 \|x 0046 \|a ebook_2022_dissbremen
995			\|2 22 \|1 01 \|x 0018 \|a SUBolrd
995			\|2 23 \|1 01 \|x 0830 \|a olr-d
995			\|2 60 \|1 01 \|x 0705 \|a OLRD
995			\|2 63 \|1 01 \|x 3401 \|a ORD
995			\|2 132 \|1 01 \|x 0959 \|a OLR-DISS
995			\|2 151 \|1 01 \|x 0546 \|a OLR-ODISS
995			\|2 161 \|1 01 \|x 0960 \|a ORD
995			\|2 293 \|1 01 \|x 3293 \|a ORD
998			\|2 23 \|1 01 \|x 0830 \|0 2024-10-12 10:31:16

Indexfelder

author_variant	j z jz
matchkey_str	zhangjunlikopfachimbehrmannjanhinrich:2021----:uniiainfoersuenudcinoeadtipiainotelp
oclc_num	1311518074
hierarchy_sort_str	2021
publishDate	2021
allfields	urn:nbn:de:gbv:46-elib58150 urn 10.26092/elib/1438 doi (DE-627)1797019651 (DE-599)KXP1797019651 (OCoLC)1311518074 DE-627 ger DE-627 rda eng XA-DE-HB 551.22 DE-101 550 DE-101 Zhang, Junli verfasserin (orcid)0000-0002-2546-8633 aut Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang Bremen 2021 1 Online-Ressource (124 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2021 In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs. Archivierung/Langzeitarchivierung gewährleistet PEHB XA-DE-HB pdager DE-46 pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Kopf, Achim akademischer betreuerin (DE-588)1057165131 (DE-627)795691181 (DE-576)413695298 dgs Behrmann, Jan Hinrich 1953- akademischer betreuerin (DE-588)143664867 (DE-627)653840470 (DE-576)338247793 dgs Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Zhang, Junli Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface Bremen, 2021 124 Seiten (DE-627)1797019996 http://dx.doi.org/10.26092/elib/1438 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 Resolving-System kostenfrei https://d-nb.info/1338948229/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://media.suub.uni-bremen.de/handle/elib/5815 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER DSpace BO 20 01 0084 4593077184 x 12-10-24 21 01 0046 4106904322 ebook_2022_dissbremen Kostenloser Zugriff zza 30-03-22 22 01 0018 4593180066 SUBolrd xu 12-10-24 23 01 0830 459322912X olr-d x 12-10-24 30 01 0104 4593276152 z 12-10-24 40 01 0007 4593309697 xsn 12-10-24 60 01 0705 4593367433 OLRD z 12-10-24 63 01 3401 4593423171 ORD x 12-10-24 70 01 0089 4593474175 z 12-10-24 105 01 0841 4593865778 z 12-10-24 110 01 3110 4593578078 x 12-10-24 132 01 0959 4593621836 OLR-DISS x 12-10-24 151 01 0546 4593664993 OLR-ODISS z 12-10-24 161 01 0960 4593688027 ORD z 12-10-24 293 01 3293 4593815827 ORD z 12-10-24 370 01 4370 4593853710 x 12-10-24 2403 01 DE-LFER 4113689865 00 --%%-- --%%-- n --%%-- l01 08-04-22 20 01 0084 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 21 01 0046 https://doi.org/10.26092/elib/1438 LF 22 01 0018 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 23 01 0830 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 30 01 0104 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 40 01 0007 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 60 01 0705 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 63 01 3401 E-Book https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 LF 70 01 0089 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 105 01 0841 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 110 01 3110 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 132 01 0959 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 151 01 0546 Volltext https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 161 01 0960 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 293 01 3293 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 370 01 4370 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 2403 01 DE-LFER http://dx.doi.org/10.26092/elib/1438 21 00 DE-46 00 Universität Bremen 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2022_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2024-10-12 10:31:16
spelling	urn:nbn:de:gbv:46-elib58150 urn 10.26092/elib/1438 doi (DE-627)1797019651 (DE-599)KXP1797019651 (OCoLC)1311518074 DE-627 ger DE-627 rda eng XA-DE-HB 551.22 DE-101 550 DE-101 Zhang, Junli verfasserin (orcid)0000-0002-2546-8633 aut Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang Bremen 2021 1 Online-Ressource (124 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2021 In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs. Archivierung/Langzeitarchivierung gewährleistet PEHB XA-DE-HB pdager DE-46 pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Kopf, Achim akademischer betreuerin (DE-588)1057165131 (DE-627)795691181 (DE-576)413695298 dgs Behrmann, Jan Hinrich 1953- akademischer betreuerin (DE-588)143664867 (DE-627)653840470 (DE-576)338247793 dgs Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Zhang, Junli Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface Bremen, 2021 124 Seiten (DE-627)1797019996 http://dx.doi.org/10.26092/elib/1438 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 Resolving-System kostenfrei https://d-nb.info/1338948229/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://media.suub.uni-bremen.de/handle/elib/5815 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER DSpace BO 20 01 0084 4593077184 x 12-10-24 21 01 0046 4106904322 ebook_2022_dissbremen Kostenloser Zugriff zza 30-03-22 22 01 0018 4593180066 SUBolrd xu 12-10-24 23 01 0830 459322912X olr-d x 12-10-24 30 01 0104 4593276152 z 12-10-24 40 01 0007 4593309697 xsn 12-10-24 60 01 0705 4593367433 OLRD z 12-10-24 63 01 3401 4593423171 ORD x 12-10-24 70 01 0089 4593474175 z 12-10-24 105 01 0841 4593865778 z 12-10-24 110 01 3110 4593578078 x 12-10-24 132 01 0959 4593621836 OLR-DISS x 12-10-24 151 01 0546 4593664993 OLR-ODISS z 12-10-24 161 01 0960 4593688027 ORD z 12-10-24 293 01 3293 4593815827 ORD z 12-10-24 370 01 4370 4593853710 x 12-10-24 2403 01 DE-LFER 4113689865 00 --%%-- --%%-- n --%%-- l01 08-04-22 20 01 0084 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 21 01 0046 https://doi.org/10.26092/elib/1438 LF 22 01 0018 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 23 01 0830 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 30 01 0104 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 40 01 0007 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 60 01 0705 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 63 01 3401 E-Book https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 LF 70 01 0089 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 105 01 0841 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 110 01 3110 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 132 01 0959 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 151 01 0546 Volltext https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 161 01 0960 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 293 01 3293 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 370 01 4370 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 2403 01 DE-LFER http://dx.doi.org/10.26092/elib/1438 21 00 DE-46 00 Universität Bremen 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2022_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2024-10-12 10:31:16
allfields_unstemmed	urn:nbn:de:gbv:46-elib58150 urn 10.26092/elib/1438 doi (DE-627)1797019651 (DE-599)KXP1797019651 (OCoLC)1311518074 DE-627 ger DE-627 rda eng XA-DE-HB 551.22 DE-101 550 DE-101 Zhang, Junli verfasserin (orcid)0000-0002-2546-8633 aut Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang Bremen 2021 1 Online-Ressource (124 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2021 In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs. Archivierung/Langzeitarchivierung gewährleistet PEHB XA-DE-HB pdager DE-46 pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Kopf, Achim akademischer betreuerin (DE-588)1057165131 (DE-627)795691181 (DE-576)413695298 dgs Behrmann, Jan Hinrich 1953- akademischer betreuerin (DE-588)143664867 (DE-627)653840470 (DE-576)338247793 dgs Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Zhang, Junli Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface Bremen, 2021 124 Seiten (DE-627)1797019996 http://dx.doi.org/10.26092/elib/1438 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 Resolving-System kostenfrei https://d-nb.info/1338948229/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://media.suub.uni-bremen.de/handle/elib/5815 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER DSpace BO 20 01 0084 4593077184 x 12-10-24 21 01 0046 4106904322 ebook_2022_dissbremen Kostenloser Zugriff zza 30-03-22 22 01 0018 4593180066 SUBolrd xu 12-10-24 23 01 0830 459322912X olr-d x 12-10-24 30 01 0104 4593276152 z 12-10-24 40 01 0007 4593309697 xsn 12-10-24 60 01 0705 4593367433 OLRD z 12-10-24 63 01 3401 4593423171 ORD x 12-10-24 70 01 0089 4593474175 z 12-10-24 105 01 0841 4593865778 z 12-10-24 110 01 3110 4593578078 x 12-10-24 132 01 0959 4593621836 OLR-DISS x 12-10-24 151 01 0546 4593664993 OLR-ODISS z 12-10-24 161 01 0960 4593688027 ORD z 12-10-24 293 01 3293 4593815827 ORD z 12-10-24 370 01 4370 4593853710 x 12-10-24 2403 01 DE-LFER 4113689865 00 --%%-- --%%-- n --%%-- l01 08-04-22 20 01 0084 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 21 01 0046 https://doi.org/10.26092/elib/1438 LF 22 01 0018 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 23 01 0830 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 30 01 0104 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 40 01 0007 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 60 01 0705 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 63 01 3401 E-Book https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 LF 70 01 0089 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 105 01 0841 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 110 01 3110 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 132 01 0959 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 151 01 0546 Volltext https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 161 01 0960 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 293 01 3293 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 370 01 4370 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 2403 01 DE-LFER http://dx.doi.org/10.26092/elib/1438 21 00 DE-46 00 Universität Bremen 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2022_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2024-10-12 10:31:16
allfieldsGer	urn:nbn:de:gbv:46-elib58150 urn 10.26092/elib/1438 doi (DE-627)1797019651 (DE-599)KXP1797019651 (OCoLC)1311518074 DE-627 ger DE-627 rda eng XA-DE-HB 551.22 DE-101 550 DE-101 Zhang, Junli verfasserin (orcid)0000-0002-2546-8633 aut Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang Bremen 2021 1 Online-Ressource (124 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2021 In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs. Archivierung/Langzeitarchivierung gewährleistet PEHB XA-DE-HB pdager DE-46 pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Kopf, Achim akademischer betreuerin (DE-588)1057165131 (DE-627)795691181 (DE-576)413695298 dgs Behrmann, Jan Hinrich 1953- akademischer betreuerin (DE-588)143664867 (DE-627)653840470 (DE-576)338247793 dgs Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Zhang, Junli Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface Bremen, 2021 124 Seiten (DE-627)1797019996 http://dx.doi.org/10.26092/elib/1438 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 Resolving-System kostenfrei https://d-nb.info/1338948229/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://media.suub.uni-bremen.de/handle/elib/5815 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER DSpace BO 20 01 0084 4593077184 x 12-10-24 21 01 0046 4106904322 ebook_2022_dissbremen Kostenloser Zugriff zza 30-03-22 22 01 0018 4593180066 SUBolrd xu 12-10-24 23 01 0830 459322912X olr-d x 12-10-24 30 01 0104 4593276152 z 12-10-24 40 01 0007 4593309697 xsn 12-10-24 60 01 0705 4593367433 OLRD z 12-10-24 63 01 3401 4593423171 ORD x 12-10-24 70 01 0089 4593474175 z 12-10-24 105 01 0841 4593865778 z 12-10-24 110 01 3110 4593578078 x 12-10-24 132 01 0959 4593621836 OLR-DISS x 12-10-24 151 01 0546 4593664993 OLR-ODISS z 12-10-24 161 01 0960 4593688027 ORD z 12-10-24 293 01 3293 4593815827 ORD z 12-10-24 370 01 4370 4593853710 x 12-10-24 2403 01 DE-LFER 4113689865 00 --%%-- --%%-- n --%%-- l01 08-04-22 20 01 0084 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 21 01 0046 https://doi.org/10.26092/elib/1438 LF 22 01 0018 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 23 01 0830 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 30 01 0104 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 40 01 0007 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 60 01 0705 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 63 01 3401 E-Book https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 LF 70 01 0089 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 105 01 0841 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 110 01 3110 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 132 01 0959 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 151 01 0546 Volltext https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 161 01 0960 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 293 01 3293 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 370 01 4370 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 2403 01 DE-LFER http://dx.doi.org/10.26092/elib/1438 21 00 DE-46 00 Universität Bremen 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2022_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2024-10-12 10:31:16
allfieldsSound	urn:nbn:de:gbv:46-elib58150 urn 10.26092/elib/1438 doi (DE-627)1797019651 (DE-599)KXP1797019651 (OCoLC)1311518074 DE-627 ger DE-627 rda eng XA-DE-HB 551.22 DE-101 550 DE-101 Zhang, Junli verfasserin (orcid)0000-0002-2546-8633 aut Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang Bremen 2021 1 Online-Ressource (124 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2021 In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs. Archivierung/Langzeitarchivierung gewährleistet PEHB XA-DE-HB pdager DE-46 pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Kopf, Achim akademischer betreuerin (DE-588)1057165131 (DE-627)795691181 (DE-576)413695298 dgs Behrmann, Jan Hinrich 1953- akademischer betreuerin (DE-588)143664867 (DE-627)653840470 (DE-576)338247793 dgs Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Zhang, Junli Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface Bremen, 2021 124 Seiten (DE-627)1797019996 http://dx.doi.org/10.26092/elib/1438 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 Resolving-System kostenfrei https://d-nb.info/1338948229/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://media.suub.uni-bremen.de/handle/elib/5815 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER DSpace BO 20 01 0084 4593077184 x 12-10-24 21 01 0046 4106904322 ebook_2022_dissbremen Kostenloser Zugriff zza 30-03-22 22 01 0018 4593180066 SUBolrd xu 12-10-24 23 01 0830 459322912X olr-d x 12-10-24 30 01 0104 4593276152 z 12-10-24 40 01 0007 4593309697 xsn 12-10-24 60 01 0705 4593367433 OLRD z 12-10-24 63 01 3401 4593423171 ORD x 12-10-24 70 01 0089 4593474175 z 12-10-24 105 01 0841 4593865778 z 12-10-24 110 01 3110 4593578078 x 12-10-24 132 01 0959 4593621836 OLR-DISS x 12-10-24 151 01 0546 4593664993 OLR-ODISS z 12-10-24 161 01 0960 4593688027 ORD z 12-10-24 293 01 3293 4593815827 ORD z 12-10-24 370 01 4370 4593853710 x 12-10-24 2403 01 DE-LFER 4113689865 00 --%%-- --%%-- n --%%-- l01 08-04-22 20 01 0084 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 21 01 0046 https://doi.org/10.26092/elib/1438 LF 22 01 0018 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 23 01 0830 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 30 01 0104 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 40 01 0007 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 60 01 0705 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 63 01 3401 E-Book https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 LF 70 01 0089 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 105 01 0841 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 110 01 3110 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 132 01 0959 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 151 01 0546 Volltext https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 161 01 0960 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 293 01 3293 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 370 01 4370 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 2403 01 DE-LFER http://dx.doi.org/10.26092/elib/1438 21 00 DE-46 00 Universität Bremen 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2022_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2024-10-12 10:31:16
language	English
format_phy_str_mv	Book
building	20 21:z 22:u 23 30 40:s 60 63 70 105 110 132 151 161 293 370 2403:0
institution	findex.gbv.de
selectbib_iln_str_mv	20@ 21@za 22@u 23@ 30@ 40@sn 60@ 63@ 70@ 105@ 110@ 132@ 151@ 161@ 293@ 370@ 2403@01
topic_facet	pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones
hochschulschrift_txt_mv	Dissertation Universität Bremen 2021
sw_local_iln_str_mv	21:Universität Bremen DE-46:Universität Bremen
dewey-raw	551.22
isfreeaccess_bool	true
authorswithroles_txt_mv	Zhang, Junli @@aut@@ Kopf, Achim @@dgs@@ Behrmann, Jan Hinrich @@dgs@@
publishDateDaySort_date	2021-01-01T00:00:00Z
dewey-sort	3551.22
id	1797019651
genre_facet	Hochschulschrift
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a2200265 4500</leader><controlfield tag="001">1797019651</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240912025502.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220330s2021 gw \|\|\|\|\|om 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">urn:nbn:de:gbv:46-elib58150</subfield><subfield code="2">urn</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.26092/elib/1438</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)1797019651</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)KXP1797019651</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1311518074</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-DE-HB</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">551.22</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, Junli</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-2546-8633</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface</subfield><subfield code="c">submitted by Junli Zhang</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Bremen</subfield><subfield code="c">2021</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (124 Seiten)</subfield><subfield code="b">Illustrationen</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="b">Dissertation</subfield><subfield code="c">Universität Bremen</subfield><subfield code="d">2021</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs.</subfield></datafield><datafield tag="583" ind1="1" ind2=" "><subfield code="a">Archivierung/Langzeitarchivierung gewährleistet</subfield><subfield code="f">PEHB</subfield><subfield code="x">XA-DE-HB</subfield><subfield code="2">pdager</subfield><subfield code="5">DE-46</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">pore pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">consolidation experiments</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">tsunamigenic earthquakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">slow slip events</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">subduction zones</subfield></datafield><datafield tag="655" ind1=" " ind2="7"><subfield code="a">Hochschulschrift</subfield><subfield code="0">(DE-588)4113937-9</subfield><subfield code="0">(DE-627)105825778</subfield><subfield code="0">(DE-576)209480580</subfield><subfield code="2">gnd-content</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kopf, Achim</subfield><subfield code="e">akademischer betreuerin</subfield><subfield code="0">(DE-588)1057165131</subfield><subfield code="0">(DE-627)795691181</subfield><subfield code="0">(DE-576)413695298</subfield><subfield code="4">dgs</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Behrmann, Jan Hinrich</subfield><subfield code="d">1953-</subfield><subfield code="e">akademischer betreuerin</subfield><subfield code="0">(DE-588)143664867</subfield><subfield code="0">(DE-627)653840470</subfield><subfield code="0">(DE-576)338247793</subfield><subfield code="4">dgs</subfield></datafield><datafield tag="710" ind1="2" ind2=" "><subfield code="a">Universität Bremen</subfield><subfield code="e">Grad-verleihende Institution</subfield><subfield code="0">(DE-588)2001386-3</subfield><subfield code="0">(DE-627)101380429</subfield><subfield code="0">(DE-576)191575038</subfield><subfield code="4">dgg</subfield></datafield><datafield tag="751" ind1=" " ind2=" "><subfield code="a">Bremen</subfield><subfield code="0">(DE-588)4008135-7</subfield><subfield code="0">(DE-627)106369636</subfield><subfield code="0">(DE-576)208874569</subfield><subfield code="4">uvp</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="a">Zhang, Junli</subfield><subfield code="t">Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface</subfield><subfield code="d">Bremen, 2021</subfield><subfield code="h">124 Seiten</subfield><subfield code="w">(DE-627)1797019996</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.26092/elib/1438</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://d-nb.info/1338948229/34</subfield><subfield code="x">Langzeitarchivierung Nationalbibliothek</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://media.suub.uni-bremen.de/handle/elib/5815</subfield><subfield code="x">Verlag</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV-ODiss</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_1</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_KXP</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-46</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-18</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-830</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-104</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-7</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-705</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-Wim2</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-89</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-841</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-Luen4</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_132</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-959</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-546</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-960</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-960-3</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-1373</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2403</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-LFER</subfield></datafield><datafield tag="935" ind1=" " ind2=" "><subfield code="i">DSpace</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">BO</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="b">4593077184</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">01</subfield><subfield code="x">0046</subfield><subfield code="b">4106904322</subfield><subfield code="h">ebook_2022_dissbremen</subfield><subfield code="k">Kostenloser Zugriff</subfield><subfield code="y">zza</subfield><subfield code="z">30-03-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="b">4593180066</subfield><subfield code="h">SUBolrd</subfield><subfield code="y">xu</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="b">459322912X</subfield><subfield code="h">olr-d</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">30</subfield><subfield code="1">01</subfield><subfield code="x">0104</subfield><subfield code="b">4593276152</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">40</subfield><subfield code="1">01</subfield><subfield code="x">0007</subfield><subfield code="b">4593309697</subfield><subfield code="y">xsn</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="b">4593367433</subfield><subfield code="h">OLRD</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="b">4593423171</subfield><subfield code="h">ORD</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">70</subfield><subfield code="1">01</subfield><subfield code="x">0089</subfield><subfield code="b">4593474175</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">105</subfield><subfield code="1">01</subfield><subfield code="x">0841</subfield><subfield code="b">4593865778</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="b">4593578078</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">132</subfield><subfield code="1">01</subfield><subfield code="x">0959</subfield><subfield code="b">4593621836</subfield><subfield code="h">OLR-DISS</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">151</subfield><subfield code="1">01</subfield><subfield code="x">0546</subfield><subfield code="b">4593664993</subfield><subfield code="h">OLR-ODISS</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="b">4593688027</subfield><subfield code="h">ORD</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="b">4593815827</subfield><subfield code="h">ORD</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="b">4593853710</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2403</subfield><subfield code="1">01</subfield><subfield code="x">DE-LFER</subfield><subfield code="b">4113689865</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">n</subfield><subfield code="j">--%%--</subfield><subfield code="y">l01</subfield><subfield code="z">08-04-22</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">01</subfield><subfield code="x">0046</subfield><subfield code="r">https://doi.org/10.26092/elib/1438</subfield><subfield code="z">LF</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">30</subfield><subfield code="1">01</subfield><subfield code="x">0104</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">40</subfield><subfield code="1">01</subfield><subfield code="x">0007</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="y">E-Book</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield><subfield code="z">LF</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">70</subfield><subfield code="1">01</subfield><subfield code="x">0089</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">105</subfield><subfield code="1">01</subfield><subfield code="x">0841</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">132</subfield><subfield code="1">01</subfield><subfield code="x">0959</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">151</subfield><subfield code="1">01</subfield><subfield code="x">0546</subfield><subfield code="y">Volltext</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">2403</subfield><subfield code="1">01</subfield><subfield code="x">DE-LFER</subfield><subfield code="r">http://dx.doi.org/10.26092/elib/1438</subfield></datafield><datafield tag="982" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">00</subfield><subfield code="x">DE-46</subfield><subfield code="8">00</subfield><subfield code="a">Universität Bremen</subfield></datafield><datafield tag="983" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="8">10</subfield><subfield code="a">ho</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">01</subfield><subfield code="x">0046</subfield><subfield code="a">ebook_2022_dissbremen</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="a">SUBolrd</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="a">olr-d</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="a">ORD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">132</subfield><subfield code="1">01</subfield><subfield code="x">0959</subfield><subfield code="a">OLR-DISS</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">151</subfield><subfield code="1">01</subfield><subfield code="x">0546</subfield><subfield code="a">OLR-ODISS</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="a">ORD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="a">ORD</subfield></datafield><datafield tag="998" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="0">2024-10-12 10:31:16</subfield></datafield></record></collection>
standort_str_mv	--%%--
standort_iln_str_mv	2403:--%%-- DE-LFER:--%%--
author	Zhang, Junli
spellingShingle	Zhang, Junli ddc 551.22 ddc 550 misc pore pressure misc consolidation experiments misc tsunamigenic earthquakes misc slow slip events misc subduction zones 21 Universität Bremen Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface
authorStr	Zhang, Junli
ppnlink_with_tag_str_mv	@@776@@(DE-627)1797019996
format	eBook
dewey-ones	551 - Geology, hydrology & meteorology 550 - Earth sciences
delete_txt_mv	keep
author_role	aut
collection	KXP GVK SWB
publishPlace	Bremen
remote_str	true
abrufzeichen_iln_str_mv	21@ebook_2022_dissbremen 22@SUBolrd 23@olr-d 60@OLRD 63@ORD 132@OLR-DISS 151@OLR-ODISS 161@ORD 293@ORD
abrufzeichen_iln_scis_mv	21@ebook_2022_dissbremen 22@SUBolrd 23@olr-d 60@OLRD 63@ORD 132@OLR-DISS 151@OLR-ODISS 161@ORD 293@ORD
last_changed_iln_str_mv	20@12-10-24 21@30-03-22 22@12-10-24 23@12-10-24 30@12-10-24 40@12-10-24 60@12-10-24 63@12-10-24 70@12-10-24 105@12-10-24 110@12-10-24 132@12-10-24 151@12-10-24 161@12-10-24 293@12-10-24 370@12-10-24 2403@08-04-22
illustrated	Not Illustrated
notation_local_iln_str_mv	60:ho 0705:ho
topic_title	551.22 DE-101 550 DE-101 21 00 DE-46 00 Universität Bremen Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang pore pressure consolidation experiments tsunamigenic earthquakes slow slip events subduction zones
topic	ddc 551.22 ddc 550 misc pore pressure misc consolidation experiments misc tsunamigenic earthquakes misc slow slip events misc subduction zones 21 Universität Bremen
topic_unstemmed	ddc 551.22 ddc 550 misc pore pressure misc consolidation experiments misc tsunamigenic earthquakes misc slow slip events misc subduction zones 21 Universität Bremen
topic_browse	ddc 551.22 ddc 550 misc pore pressure misc consolidation experiments misc tsunamigenic earthquakes misc slow slip events misc subduction zones 21 Universität Bremen
format_facet	Elektronische Bücher Bücher Elektronische Ressource Hochschulschriften
standort_txtP_mv	--%%--
format_main_str_mv	Text Buch
format_details_str_mv	Hochschulschrift
carriertype_str_mv	cr
author2_variant	a k ak j h b jh jhb
signature	--%%--
signature_str_mv	--%%--
dewey-tens	550 - Earth sciences & geology
isfreeaccess_txt	true
normlinkwithrole_str_mv	(DE-588)4113937-9@@655@@ (DE-588)1057165131@@dgs@@ (DE-588)143664867@@dgs@@ (DE-588)2001386-3@@dgg@@ (DE-588)4008135-7@@uvp@@
title	Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface
ctrlnum	(DE-627)1797019651 (DE-599)KXP1797019651 (OCoLC)1311518074
exemplarkommentar_str_mv	21@Kostenloser Zugriff
title_full	Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface submitted by Junli Zhang
author_sort	Zhang, Junli
callnumber-first-code	-
lang_code	eng
class_local	60 01 0705 10 ho
selektneu_str_mv	23@2024-10-12 10:31:16
isOA_bool	true
dewey-hundreds	500 - Science
recordtype	marc
genre	Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content
publishDateSort	2021
contenttype_str_mv	txt
class_local_iln	60:ho 0705:ho
author_browse	Zhang, Junli
selectkey	20:x 21:z 22:x 23:x 30:z 40:x 60:z 63:x 70:z 105:z 110:x 132:x 151:z 161:z 293:z 370:x 2403:l
physical	1 Online-Ressource (124 Seiten) Illustrationen
class	551.22 DE-101 550 DE-101 60 01 0705 10 ho
format_se	Elektronische Bücher
countryofpublication_str_mv	XA-DE-HB
author-letter	Zhang, Junli
classname_local_iln_str_mv	60: 0705:
doi_str_mv	10.26092/elib/1438
normlink	(ORCID)0000-0002-2546-8633 4113937-9 105825778 209480580 1057165131 795691181 413695298 143664867 653840470 338247793 2001386-3 101380429 191575038 4008135-7 106369636 208874569 2024-10-12 10:31:16
normlink_prefix_str_mv	(orcid)0000-0002-2546-8633 (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 (DE-588)1057165131 (DE-627)795691181 (DE-576)413695298 (DE-588)143664867 (DE-627)653840470 (DE-576)338247793 (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 2024-10-12 10:31:16
dewey-full	551.22 550
author2-role	akademischer betreuerin Grad-verleihende Institution
title_sort	quantification of pore pressure in subduction zones and its implication for the slip behavior of the plate interface
title_auth	Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface
abstract	In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs.
abstractGer	In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs.
abstract_unstemmed	In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs.
collection_details	GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER
title_short	Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface
url	http://dx.doi.org/10.26092/elib/1438 https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150 https://d-nb.info/1338948229/34 https://media.suub.uni-bremen.de/handle/elib/5815
ausleihindikator_str_mv	20 21 22 23 30 40 60 63 70 105 110 132 151 161 293 370 2403:n
rolewithnormlink_str_mv	@@655@@(DE-588)4113937-9 @@dgs@@(DE-588)1057165131 @@dgs@@(DE-588)143664867 @@dgg@@(DE-588)2001386-3 @@uvp@@(DE-588)4008135-7
remote_bool	true
author2	Kopf, Achim Behrmann, Jan Hinrich 1953- Universität Bremen
author2Str	Kopf, Achim Behrmann, Jan Hinrich 1953- Universität Bremen
ppnlink	1797019996
mediatype_str_mv	c
isOA_txt	true
hochschulschrift_bool	true
author2_role	dgs dgs
doi_str	10.26092/elib/1438
callnumber-a	--%%--
up_date	2024-10-13T07:12:57.186Z
_version_	1812781939754532864
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000cam a2200265 4500</leader><controlfield tag="001">1797019651</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240912025502.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">220330s2021 gw \|\|\|\|\|om 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">urn:nbn:de:gbv:46-elib58150</subfield><subfield code="2">urn</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.26092/elib/1438</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)1797019651</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)KXP1797019651</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)1311518074</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="044" ind1=" " ind2=" "><subfield code="c">XA-DE-HB</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">551.22</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-101</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, Junli</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-2546-8633</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface</subfield><subfield code="c">submitted by Junli Zhang</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Bremen</subfield><subfield code="c">2021</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (124 Seiten)</subfield><subfield code="b">Illustrationen</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="b">Dissertation</subfield><subfield code="c">Universität Bremen</subfield><subfield code="d">2021</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">In this Ph.D. dissertation, pore pressure in the Nankai Trough, North Sumatra, and Northern Hikurangi subduction zones is investigated through multi approaches including uniaxial consolidation experiments, porosity-based prediction equations, and fluid flow models. In the Nankai Trough subduction zone, continuous excess pore pressure is revealed in the accreted and underthrust sediments, implying the Nankai décollement is not a fluid barrier. Pore pressures 84%-93% of the lithostatic stress along the décollement are inferred and lead to extremely low shear strength at the deformation front. This increases the likelihood of a large tsunami offshore SW Japan when a large earthquake happens. In addition, a pore pressure prediction approach accounting for consolidation state of sediments is developed. Compared with the normally consolidated sediment, overconsolidated sediments in the Nankai Trough generate 40%~50% less excess pore pressure. The shear strength along the Nankai décollement is below 2.2 MPa, obviously larger than the shear stress (<0.4 MPa). This implies that the accretionary prism is not at Coulomb failure. In the North Sumatra subduction zone, moderate excess pore pressure is revealed in the proto-décollement horizon. Pore pressure modeling shows that the excess pore pressure increases continuously and reaches a high level corresponding to a pore pressure up to 96% of lithostatic stress, as the sediment approaches the trench. The high excess pore pressure explains the 2004 Sumatra earthquake. In the Northern Hikurangi subduction zone, consolidation experiments show that the trench-wedge facies are underconsolidated. Pore pressure 77% of lithostatic stress is revealed at the top of the Pāpaku fault, whereas the pore pressure at the bottom increases to 93% of lithostatic stress. Slow slip events (SSEs) are simulated under this pore pressure condition. The modeling results are comparable to the natural SSEs.</subfield></datafield><datafield tag="583" ind1="1" ind2=" "><subfield code="a">Archivierung/Langzeitarchivierung gewährleistet</subfield><subfield code="f">PEHB</subfield><subfield code="x">XA-DE-HB</subfield><subfield code="2">pdager</subfield><subfield code="5">DE-46</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">pore pressure</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">consolidation experiments</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">tsunamigenic earthquakes</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">slow slip events</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">subduction zones</subfield></datafield><datafield tag="655" ind1=" " ind2="7"><subfield code="a">Hochschulschrift</subfield><subfield code="0">(DE-588)4113937-9</subfield><subfield code="0">(DE-627)105825778</subfield><subfield code="0">(DE-576)209480580</subfield><subfield code="2">gnd-content</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Kopf, Achim</subfield><subfield code="e">akademischer betreuerin</subfield><subfield code="0">(DE-588)1057165131</subfield><subfield code="0">(DE-627)795691181</subfield><subfield code="0">(DE-576)413695298</subfield><subfield code="4">dgs</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Behrmann, Jan Hinrich</subfield><subfield code="d">1953-</subfield><subfield code="e">akademischer betreuerin</subfield><subfield code="0">(DE-588)143664867</subfield><subfield code="0">(DE-627)653840470</subfield><subfield code="0">(DE-576)338247793</subfield><subfield code="4">dgs</subfield></datafield><datafield tag="710" ind1="2" ind2=" "><subfield code="a">Universität Bremen</subfield><subfield code="e">Grad-verleihende Institution</subfield><subfield code="0">(DE-588)2001386-3</subfield><subfield code="0">(DE-627)101380429</subfield><subfield code="0">(DE-576)191575038</subfield><subfield code="4">dgg</subfield></datafield><datafield tag="751" ind1=" " ind2=" "><subfield code="a">Bremen</subfield><subfield code="0">(DE-588)4008135-7</subfield><subfield code="0">(DE-627)106369636</subfield><subfield code="0">(DE-576)208874569</subfield><subfield code="4">uvp</subfield></datafield><datafield tag="776" ind1="0" ind2="8"><subfield code="i">Erscheint auch als</subfield><subfield code="n">Druck-Ausgabe</subfield><subfield code="a">Zhang, Junli</subfield><subfield code="t">Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface</subfield><subfield code="d">Bremen, 2021</subfield><subfield code="h">124 Seiten</subfield><subfield code="w">(DE-627)1797019996</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">http://dx.doi.org/10.26092/elib/1438</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield><subfield code="x">Resolving-System</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://d-nb.info/1338948229/34</subfield><subfield code="x">Langzeitarchivierung Nationalbibliothek</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://media.suub.uni-bremen.de/handle/elib/5815</subfield><subfield code="x">Verlag</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV-ODiss</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-84</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_1</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_KXP</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_21</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-46</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-18</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-830</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_30</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-104</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-7</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-705</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-Wim2</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-89</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-841</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-Luen4</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_132</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-959</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-546</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_161</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-960</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_293</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-960-3</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-1373</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2403</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ISIL_DE-LFER</subfield></datafield><datafield tag="935" ind1=" " ind2=" "><subfield code="i">DSpace</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">BO</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="b">4593077184</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">01</subfield><subfield code="x">0046</subfield><subfield code="b">4106904322</subfield><subfield code="h">ebook_2022_dissbremen</subfield><subfield code="k">Kostenloser Zugriff</subfield><subfield code="y">zza</subfield><subfield code="z">30-03-22</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="b">4593180066</subfield><subfield code="h">SUBolrd</subfield><subfield code="y">xu</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="b">459322912X</subfield><subfield code="h">olr-d</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">30</subfield><subfield code="1">01</subfield><subfield code="x">0104</subfield><subfield code="b">4593276152</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">40</subfield><subfield code="1">01</subfield><subfield code="x">0007</subfield><subfield code="b">4593309697</subfield><subfield code="y">xsn</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="b">4593367433</subfield><subfield code="h">OLRD</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="b">4593423171</subfield><subfield code="h">ORD</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">70</subfield><subfield code="1">01</subfield><subfield code="x">0089</subfield><subfield code="b">4593474175</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">105</subfield><subfield code="1">01</subfield><subfield code="x">0841</subfield><subfield code="b">4593865778</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="b">4593578078</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">132</subfield><subfield code="1">01</subfield><subfield code="x">0959</subfield><subfield code="b">4593621836</subfield><subfield code="h">OLR-DISS</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">151</subfield><subfield code="1">01</subfield><subfield code="x">0546</subfield><subfield code="b">4593664993</subfield><subfield code="h">OLR-ODISS</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="b">4593688027</subfield><subfield code="h">ORD</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="b">4593815827</subfield><subfield code="h">ORD</subfield><subfield code="y">z</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="b">4593853710</subfield><subfield code="y">x</subfield><subfield code="z">12-10-24</subfield></datafield><datafield tag="980" ind1=" " ind2=" "><subfield code="2">2403</subfield><subfield code="1">01</subfield><subfield code="x">DE-LFER</subfield><subfield code="b">4113689865</subfield><subfield code="c">00</subfield><subfield code="f">--%%--</subfield><subfield code="d">--%%--</subfield><subfield code="e">n</subfield><subfield code="j">--%%--</subfield><subfield code="y">l01</subfield><subfield code="z">08-04-22</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">01</subfield><subfield code="x">0046</subfield><subfield code="r">https://doi.org/10.26092/elib/1438</subfield><subfield code="z">LF</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">30</subfield><subfield code="1">01</subfield><subfield code="x">0104</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">40</subfield><subfield code="1">01</subfield><subfield code="x">0007</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="y">E-Book</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield><subfield code="z">LF</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">70</subfield><subfield code="1">01</subfield><subfield code="x">0089</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">105</subfield><subfield code="1">01</subfield><subfield code="x">0841</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">132</subfield><subfield code="1">01</subfield><subfield code="x">0959</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">151</subfield><subfield code="1">01</subfield><subfield code="x">0546</subfield><subfield code="y">Volltext</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="r">https://nbn-resolving.org/urn:nbn:de:gbv:46-elib58150</subfield></datafield><datafield tag="981" ind1=" " ind2=" "><subfield code="2">2403</subfield><subfield code="1">01</subfield><subfield code="x">DE-LFER</subfield><subfield code="r">http://dx.doi.org/10.26092/elib/1438</subfield></datafield><datafield tag="982" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">00</subfield><subfield code="x">DE-46</subfield><subfield code="8">00</subfield><subfield code="a">Universität Bremen</subfield></datafield><datafield tag="983" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="8">10</subfield><subfield code="a">ho</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">20</subfield><subfield code="1">01</subfield><subfield code="x">0084</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">110</subfield><subfield code="1">01</subfield><subfield code="x">3110</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="985" ind1=" " ind2=" "><subfield code="2">370</subfield><subfield code="1">01</subfield><subfield code="x">4370</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">21</subfield><subfield code="1">01</subfield><subfield code="x">0046</subfield><subfield code="a">ebook_2022_dissbremen</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">22</subfield><subfield code="1">01</subfield><subfield code="x">0018</subfield><subfield code="a">SUBolrd</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="a">olr-d</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">60</subfield><subfield code="1">01</subfield><subfield code="x">0705</subfield><subfield code="a">OLRD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">63</subfield><subfield code="1">01</subfield><subfield code="x">3401</subfield><subfield code="a">ORD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">132</subfield><subfield code="1">01</subfield><subfield code="x">0959</subfield><subfield code="a">OLR-DISS</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">151</subfield><subfield code="1">01</subfield><subfield code="x">0546</subfield><subfield code="a">OLR-ODISS</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">161</subfield><subfield code="1">01</subfield><subfield code="x">0960</subfield><subfield code="a">ORD</subfield></datafield><datafield tag="995" ind1=" " ind2=" "><subfield code="2">293</subfield><subfield code="1">01</subfield><subfield code="x">3293</subfield><subfield code="a">ORD</subfield></datafield><datafield tag="998" ind1=" " ind2=" "><subfield code="2">23</subfield><subfield code="1">01</subfield><subfield code="x">0830</subfield><subfield code="0">2024-10-12 10:31:16</subfield></datafield></record></collection>
score	6.8996325

Nicht das Richtige dabei?

Schreiben Sie uns!

Quantification of pore pressure in subduction zones and its implication for the slip behavior of the Plate Interface

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?