Submarine landslides in active margin environments : slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean

Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments....
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Strozyk, Frank [verfasserIn]
Hochschulschrift:	Bremen, Univ., Diss., 2009

Format:	E-Book
Sprache:	Englisch

Erschienen:	2010

Formangabe:	Hochschulschrift

Umfang:	Online-Ressource (PDF-Datei: 133 S., 36,5 MB)

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Strozyk, Frank: Submarine landslides in active margin environments - 2009

Links:	Link aufrufen Volltext Volltext Volltext Volltext

DOI / URN:	urn:nbn:de:gbv:46-diss000117295

Katalog-ID:	620037423

Internformat


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Indexfelder

author_variant	f s fs
matchkey_str	strozykfrank:2010----:umrnlnsieiatvmri
oclc_num	839414811
hierarchy_sort_str	2010
publishDate	2010
allfields	100079797X DE-101 urn:nbn:de:gbv:46-diss000117295 urn (DE-627)620037423 (DE-599)GBV620037423 (OCoLC)839414811 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB Strozyk, Frank verfasserin aut Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean by Frank Strozyk 2010 Online-Ressource (PDF-Datei: 133 S., 36,5 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Bremen, Univ., Diss., 2009 Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Erscheint auch als Druck-Ausgabe Strozyk, Frank Submarine landslides in active margin environments 2009 133 S (DE-627)620037334 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext http://elib.suub.uni-bremen.de/diss/docs/00011729.pdf PDF Verlag kostenfrei Volltext http://d-nb.info/100079797X/34 Langzeitarchivierung Nationalbibliothek Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO 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 BO 045F 550 20 01 0084 1180782526 x 11-09-10 21 01 0046 1116123290 zza 02-03-10 22 01 0018 1180977955 SUBolrd xu 11-09-10 23 01 0830 1181063973 olr-d x 11-09-10 30 01 0104 1181125812 z 11-09-10 40 01 0007 1181190576 xsn 11-09-10 60 01 0705 1181283396 OLRD z 11-09-10 63 01 3401 1595669264 ORD x 21-01-16 70 01 0089 1228072213 zdo 20-02-11 105 01 0841 1596482400 z 21-01-16 110 01 3110 1181371031 x 11-09-10 132 01 0959 1497543495 OLR-DISS x 11-08-14 151 01 0546 3594091554 OLR-ODISS z 13-02-20 161 01 0960 1597429902 ORD x 28-01-16 293 01 3293 1597855782 ORD xf 28-01-16 370 01 4370 118141542X x 11-09-10 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 00 DE-46 99 07 40 00 DE-7 00 (DE-627)625046323 VAE 880 Passive und aktive Kontinentalränder {Tektonik} 40 00 DE-7 01 (DE-627)623606259 TSF 300 Griechenland und griechische Inseln {Geophysik} 40 00 DE-7 02 (DE-627)623607069 TSZ 100 Atlantischer Ozean {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 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 2010-09-11:05:41:15
spelling	100079797X DE-101 urn:nbn:de:gbv:46-diss000117295 urn (DE-627)620037423 (DE-599)GBV620037423 (OCoLC)839414811 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB Strozyk, Frank verfasserin aut Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean by Frank Strozyk 2010 Online-Ressource (PDF-Datei: 133 S., 36,5 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Bremen, Univ., Diss., 2009 Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Erscheint auch als Druck-Ausgabe Strozyk, Frank Submarine landslides in active margin environments 2009 133 S (DE-627)620037334 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext http://elib.suub.uni-bremen.de/diss/docs/00011729.pdf PDF Verlag kostenfrei Volltext http://d-nb.info/100079797X/34 Langzeitarchivierung Nationalbibliothek Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO 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 BO 045F 550 20 01 0084 1180782526 x 11-09-10 21 01 0046 1116123290 zza 02-03-10 22 01 0018 1180977955 SUBolrd xu 11-09-10 23 01 0830 1181063973 olr-d x 11-09-10 30 01 0104 1181125812 z 11-09-10 40 01 0007 1181190576 xsn 11-09-10 60 01 0705 1181283396 OLRD z 11-09-10 63 01 3401 1595669264 ORD x 21-01-16 70 01 0089 1228072213 zdo 20-02-11 105 01 0841 1596482400 z 21-01-16 110 01 3110 1181371031 x 11-09-10 132 01 0959 1497543495 OLR-DISS x 11-08-14 151 01 0546 3594091554 OLR-ODISS z 13-02-20 161 01 0960 1597429902 ORD x 28-01-16 293 01 3293 1597855782 ORD xf 28-01-16 370 01 4370 118141542X x 11-09-10 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 00 DE-46 99 07 40 00 DE-7 00 (DE-627)625046323 VAE 880 Passive und aktive Kontinentalränder {Tektonik} 40 00 DE-7 01 (DE-627)623606259 TSF 300 Griechenland und griechische Inseln {Geophysik} 40 00 DE-7 02 (DE-627)623607069 TSZ 100 Atlantischer Ozean {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 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 2010-09-11:05:41:15
allfields_unstemmed	100079797X DE-101 urn:nbn:de:gbv:46-diss000117295 urn (DE-627)620037423 (DE-599)GBV620037423 (OCoLC)839414811 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB Strozyk, Frank verfasserin aut Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean by Frank Strozyk 2010 Online-Ressource (PDF-Datei: 133 S., 36,5 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Bremen, Univ., Diss., 2009 Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Erscheint auch als Druck-Ausgabe Strozyk, Frank Submarine landslides in active margin environments 2009 133 S (DE-627)620037334 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext http://elib.suub.uni-bremen.de/diss/docs/00011729.pdf PDF Verlag kostenfrei Volltext http://d-nb.info/100079797X/34 Langzeitarchivierung Nationalbibliothek Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO 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 BO 045F 550 20 01 0084 1180782526 x 11-09-10 21 01 0046 1116123290 zza 02-03-10 22 01 0018 1180977955 SUBolrd xu 11-09-10 23 01 0830 1181063973 olr-d x 11-09-10 30 01 0104 1181125812 z 11-09-10 40 01 0007 1181190576 xsn 11-09-10 60 01 0705 1181283396 OLRD z 11-09-10 63 01 3401 1595669264 ORD x 21-01-16 70 01 0089 1228072213 zdo 20-02-11 105 01 0841 1596482400 z 21-01-16 110 01 3110 1181371031 x 11-09-10 132 01 0959 1497543495 OLR-DISS x 11-08-14 151 01 0546 3594091554 OLR-ODISS z 13-02-20 161 01 0960 1597429902 ORD x 28-01-16 293 01 3293 1597855782 ORD xf 28-01-16 370 01 4370 118141542X x 11-09-10 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 00 DE-46 99 07 40 00 DE-7 00 (DE-627)625046323 VAE 880 Passive und aktive Kontinentalränder {Tektonik} 40 00 DE-7 01 (DE-627)623606259 TSF 300 Griechenland und griechische Inseln {Geophysik} 40 00 DE-7 02 (DE-627)623607069 TSZ 100 Atlantischer Ozean {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 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 2010-09-11:05:41:15
allfieldsGer	100079797X DE-101 urn:nbn:de:gbv:46-diss000117295 urn (DE-627)620037423 (DE-599)GBV620037423 (OCoLC)839414811 DE-627 ger DE-627 rakwb eng XA-DE 550 OCLC 550 DNB Strozyk, Frank verfasserin aut Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean by Frank Strozyk 2010 Online-Ressource (PDF-Datei: 133 S., 36,5 MB) Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Bremen, Univ., Diss., 2009 Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings. Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Bremen uvp Erscheint auch als Druck-Ausgabe Strozyk, Frank Submarine landslides in active margin environments 2009 133 S (DE-627)620037334 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext http://elib.suub.uni-bremen.de/diss/docs/00011729.pdf PDF Verlag kostenfrei Volltext http://d-nb.info/100079797X/34 Langzeitarchivierung Nationalbibliothek Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 Resolving-System Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GEO SSG-OPC-GGO 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 BO 045F 550 20 01 0084 1180782526 x 11-09-10 21 01 0046 1116123290 zza 02-03-10 22 01 0018 1180977955 SUBolrd xu 11-09-10 23 01 0830 1181063973 olr-d x 11-09-10 30 01 0104 1181125812 z 11-09-10 40 01 0007 1181190576 xsn 11-09-10 60 01 0705 1181283396 OLRD z 11-09-10 63 01 3401 1595669264 ORD x 21-01-16 70 01 0089 1228072213 zdo 20-02-11 105 01 0841 1596482400 z 21-01-16 110 01 3110 1181371031 x 11-09-10 132 01 0959 1497543495 OLR-DISS x 11-08-14 151 01 0546 3594091554 OLR-ODISS z 13-02-20 161 01 0960 1597429902 ORD x 28-01-16 293 01 3293 1597855782 ORD xf 28-01-16 370 01 4370 118141542X x 11-09-10 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 LF 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 21 00 DE-46 99 07 40 00 DE-7 00 (DE-627)625046323 VAE 880 Passive und aktive Kontinentalränder {Tektonik} 40 00 DE-7 01 (DE-627)623606259 TSF 300 Griechenland und griechische Inseln {Geophysik} 40 00 DE-7 02 (DE-627)623607069 TSZ 100 Atlantischer Ozean {Geophysik} 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 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 2010-09-11:05:41:15
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author	Strozyk, Frank
spellingShingle	Strozyk, Frank ddc 550 Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean
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topic_title	550 OCLC 550 DNB Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean by Frank Strozyk
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title	Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean
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title_sub	slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean
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title_sort	submarine landslides in active margin environmentsslope stability vs. neotectonic activity on the northeastern margin of crete, eastern mediterranean
title_auth	Submarine landslides in active margin environments slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean
abstract	Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings.
abstractGer	Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings.
abstract_unstemmed	Submarine landslide, slope failure, earthquake trigger, Cretan Sea, eastern Mediterranean. - This thesis is a study of the processes and factors that may govern submarine slope destabilization and mass movement as well as a slope's resistance to failure in submarine active margin environments. Prior studies on this topic in active margin settings (e.g., western North America) have shown that their slopes can be peculiar, poorly understood systems with a low recurrence of slope collapse despite the paradigm of extensive, diffuse, and widespread mass movement generally associated with the tectonic activity. The focus of this study is the active margin present along the northeast margin of Crete in the Hellenic subduction zone of the eastern Mediterranean. The previously unknown distribution and recurrence rate of landslides, their failure and transport kinematics, as well as the trigger mechanisms required for sediment instability along the northeast Cretan margin are thus investigated and reconstructed. Such data help answer the open questions related to such active margin settings.
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title_short	Submarine landslides in active margin environments
url	http://nbn-resolving.de/urn:nbn:de:gbv:46-diss000117295 http://elib.suub.uni-bremen.de/diss/docs/00011729.pdf http://d-nb.info/100079797X/34
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up_date	2024-07-11T09:10:02.241Z
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Submarine landslides in active margin environments : slope stability vs. neotectonic activity on the northeastern margin of Crete, eastern Mediterranean

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