Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand)
Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample re...
Ausführliche Beschreibung
Autor*in: |
Schwarze, Cornelius - 1988- [verfasserIn] Kukowski, Nina - 1960- [akademischer betreuerIn] Schmitt, Axel Karl - 1968- [akademischer betreuerIn] |
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Körperschaften: |
Friedrich-Schiller-Universität Jena [Grad-verleihende Institution] |
Hochschulschrift: |
Dissertation ; Friedrich-Schiller-Universität Jena ; 2022 |
Format: |
E-Book |
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Sprache: |
Englisch ; Deutsch |
Erschienen: |
Jena: 2022? |
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Schlagwörter: |
Neuseeland / Forearc-Becken / Akkretionskeil / Subduktion / Submarine Gleitung / Deformation, Geologie Meeresgeologie / Tiefseeberg / Tiefseegraben / Wechselwirkung |
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Formangabe: |
Hochschulschrift |
Anmerkung: |
Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 |
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Umfang: |
1 Online-Ressource (XVII, 141 Seiten + Anhang) ; Illustrationen, Diagramme |
Weitere Ausgabe: |
Erscheint auch als Druck-Ausgabe Schwarze, Cornelius, 1988 -: Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) - Jena, 2022 |
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Links: |
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DOI / URN: |
urn:nbn:de:gbv:27-dbt-20220505-145014-009 |
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Katalog-ID: |
1801169950 |
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520 | |a Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. | ||
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title_auth |
Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) |
abstract |
Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 |
abstractGer |
Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 |
abstract_unstemmed |
Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 |
url |
https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 https://d-nb.info/1322364494/34 https://www.db-thueringen.de/receive/dbt_mods_00051941 |
author2 |
Kukowski, Nina 1960- Schmitt, Axel Karl 1968- Friedrich-Schiller-Universität Jena |
author2Str |
Kukowski, Nina 1960- Schmitt, Axel Karl 1968- Friedrich-Schiller-Universität Jena |
ppnlink |
1801047839 |
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hochschulschrift_bool |
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author2_role |
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[2022?] |
bklnumber |
38.36 38.41 38.19 |
allfields |
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Cornelius Octavian Schwarze Jena [2022?] 1 Online-Ressource (XVII, 141 Seiten + Anhang) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 Dissertation Friedrich-Schiller-Universität Jena 2022 Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. 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spelling |
urn:nbn:de:gbv:27-dbt-20220505-145014-009 urn (DE-627)1801169950 (DE-599)KXP1801169950 (OCoLC)1314887796 DE-627 ger DE-627 rda eng ger XA-DE-TH 551.136 DE-101 550 DE-101 38.36 bkl 38.41 bkl 38.19 bkl Schwarze, Cornelius 1988- verfasserin (DE-588)1256892106 (DE-627)1801046514 aut Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) von Dipl.-Geophys. Cornelius Octavian Schwarze Jena [2022?] 1 Online-Ressource (XVII, 141 Seiten + Anhang) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 Dissertation Friedrich-Schiller-Universität Jena 2022 Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Zusammenfassungen in deutscher und englischer Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4041915-0 (DE-627)106216899 (DE-576)209047615 Neuseeland gnd s (DE-588)4334619-4 (DE-627)148298354 (DE-576)211350044 Forearc-Becken gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4384538-1 (DE-627)187467080 (DE-576)21188118X Submarine Gleitung gnd s (DE-588)4409345-7 (DE-627)198336772 (DE-576)21214555X Deformation Geologie gnd (DE-627) s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4194294-2 (DE-627)105220574 (DE-576)210093102 Tiefseeberg gnd s (DE-588)4463868-1 (DE-627)231348444 (DE-576)212701118 Tiefseegraben gnd s (DE-588)4064937-4 (DE-627)104297778 (DE-576)209155922 Wechselwirkung gnd (DE-627) Kukowski, Nina 1960- akademischer betreuerin (DE-588)17220092X (DE-627)697114465 (DE-576)133070980 dgs Schmitt, Axel Karl 1968- akademischer betreuerin (DE-588)121915506 (DE-627)705701522 (DE-576)292990308 dgs Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Schwarze, Cornelius, 1988 - Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) Jena, 2022 XVII, 141 Seiten (DE-627)1801047839 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 Langzeitarchivierung Resolving-System kostenfrei https://d-nb.info/1322364494/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://www.db-thueringen.de/receive/dbt_mods_00051941 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OLC-PHA 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_31 ISIL_DE-27 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_381 ISIL_DE-Ki130 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER 38.36 Tektonik (DE-627)106407147 38.41 Sedimentation (DE-627)106407090 38.19 Historische Geologie: Sonstiges (DE-627)106408232 BO 20 01 0084 4508104533 x 08-04-24 21 01 0046 4508121098 z 08-04-24 22 01 0018 4508137857 SUBolrd xu 08-04-24 23 01 0830 4508154522 olr-d x 08-04-24 30 01 0104 4508164072 z 08-04-24 31 01 0027 4130242407 z 09-05-22 40 01 0007 4508172032 xsn 08-04-24 60 01 0705 4508188567 OLRD z 08-04-24 63 01 3401 4508205364 ORD x 08-04-24 70 01 0089 4508213030 zdo 08-04-24 105 01 0841 4508358292 z 08-04-24 110 01 3110 4508222862 x 08-04-24 132 01 0959 4508232825 OLR-DISS x 08-04-24 151 01 0546 4508249728 OLR-ODISS z 08-04-24 161 01 0960 4508255671 ORD z 08-04-24 293 01 3293 4508289584 ORD z 08-04-24 370 01 4370 4508299407 x 08-04-24 381 01 4381 4569385168 z 21-08-24 2027 01 DE-105 4135924972 00 --%%-- Dn --%%-- --%%-- l01 18-05-22 2403 01 DE-LFER 4143595974 00 --%%-- --%%-- n --%%-- l01 07-06-22 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 01 0027 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 40 01 0007 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 381 01 4381 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 381 00 DE-Ki130 00 Seamount 381 00 DE-Ki130 00 Subduction 381 00 DE-Ki130 00 Landslide 381 00 DE-Ki130 00 Hikurangi Margin 381 00 DE-Ki130 00 New Zealand 381 00 DE-Ki130 00 Online publication 381 00 DE-Ki130 00 Dissertation 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 2027 01 DE-105 00 (DE-627)1298242568 DK 551.435.62 2027 01 DE-105 00 (DE-627)1294054791 DK 551.242.4 2027 01 DE-105 00 (DE-627)1297637046 DK 551.462.6 2027 01 DE-105 00 (DE-627)1293787280 DK 919.31 2027 01 DE-105 00 (DE-627)129278105X DK 378.245 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 2024-04-08 07:43:14 |
allfields_unstemmed |
urn:nbn:de:gbv:27-dbt-20220505-145014-009 urn (DE-627)1801169950 (DE-599)KXP1801169950 (OCoLC)1314887796 DE-627 ger DE-627 rda eng ger XA-DE-TH 551.136 DE-101 550 DE-101 38.36 bkl 38.41 bkl 38.19 bkl Schwarze, Cornelius 1988- verfasserin (DE-588)1256892106 (DE-627)1801046514 aut Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) von Dipl.-Geophys. Cornelius Octavian Schwarze Jena [2022?] 1 Online-Ressource (XVII, 141 Seiten + Anhang) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 Dissertation Friedrich-Schiller-Universität Jena 2022 Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Zusammenfassungen in deutscher und englischer Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4041915-0 (DE-627)106216899 (DE-576)209047615 Neuseeland gnd s (DE-588)4334619-4 (DE-627)148298354 (DE-576)211350044 Forearc-Becken gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4384538-1 (DE-627)187467080 (DE-576)21188118X Submarine Gleitung gnd s (DE-588)4409345-7 (DE-627)198336772 (DE-576)21214555X Deformation Geologie gnd (DE-627) s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4194294-2 (DE-627)105220574 (DE-576)210093102 Tiefseeberg gnd s (DE-588)4463868-1 (DE-627)231348444 (DE-576)212701118 Tiefseegraben gnd s (DE-588)4064937-4 (DE-627)104297778 (DE-576)209155922 Wechselwirkung gnd (DE-627) Kukowski, Nina 1960- akademischer betreuerin (DE-588)17220092X (DE-627)697114465 (DE-576)133070980 dgs Schmitt, Axel Karl 1968- akademischer betreuerin (DE-588)121915506 (DE-627)705701522 (DE-576)292990308 dgs Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Schwarze, Cornelius, 1988 - Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) Jena, 2022 XVII, 141 Seiten (DE-627)1801047839 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 Langzeitarchivierung Resolving-System kostenfrei https://d-nb.info/1322364494/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://www.db-thueringen.de/receive/dbt_mods_00051941 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OLC-PHA 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_31 ISIL_DE-27 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_381 ISIL_DE-Ki130 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER 38.36 Tektonik (DE-627)106407147 38.41 Sedimentation (DE-627)106407090 38.19 Historische Geologie: Sonstiges (DE-627)106408232 BO 20 01 0084 4508104533 x 08-04-24 21 01 0046 4508121098 z 08-04-24 22 01 0018 4508137857 SUBolrd xu 08-04-24 23 01 0830 4508154522 olr-d x 08-04-24 30 01 0104 4508164072 z 08-04-24 31 01 0027 4130242407 z 09-05-22 40 01 0007 4508172032 xsn 08-04-24 60 01 0705 4508188567 OLRD z 08-04-24 63 01 3401 4508205364 ORD x 08-04-24 70 01 0089 4508213030 zdo 08-04-24 105 01 0841 4508358292 z 08-04-24 110 01 3110 4508222862 x 08-04-24 132 01 0959 4508232825 OLR-DISS x 08-04-24 151 01 0546 4508249728 OLR-ODISS z 08-04-24 161 01 0960 4508255671 ORD z 08-04-24 293 01 3293 4508289584 ORD z 08-04-24 370 01 4370 4508299407 x 08-04-24 381 01 4381 4569385168 z 21-08-24 2027 01 DE-105 4135924972 00 --%%-- Dn --%%-- --%%-- l01 18-05-22 2403 01 DE-LFER 4143595974 00 --%%-- --%%-- n --%%-- l01 07-06-22 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 01 0027 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 40 01 0007 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 381 01 4381 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 381 00 DE-Ki130 00 Seamount 381 00 DE-Ki130 00 Subduction 381 00 DE-Ki130 00 Landslide 381 00 DE-Ki130 00 Hikurangi Margin 381 00 DE-Ki130 00 New Zealand 381 00 DE-Ki130 00 Online publication 381 00 DE-Ki130 00 Dissertation 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 2027 01 DE-105 00 (DE-627)1298242568 DK 551.435.62 2027 01 DE-105 00 (DE-627)1294054791 DK 551.242.4 2027 01 DE-105 00 (DE-627)1297637046 DK 551.462.6 2027 01 DE-105 00 (DE-627)1293787280 DK 919.31 2027 01 DE-105 00 (DE-627)129278105X DK 378.245 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 2024-04-08 07:43:14 |
allfieldsGer |
urn:nbn:de:gbv:27-dbt-20220505-145014-009 urn (DE-627)1801169950 (DE-599)KXP1801169950 (OCoLC)1314887796 DE-627 ger DE-627 rda eng ger XA-DE-TH 551.136 DE-101 550 DE-101 38.36 bkl 38.41 bkl 38.19 bkl Schwarze, Cornelius 1988- verfasserin (DE-588)1256892106 (DE-627)1801046514 aut Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) von Dipl.-Geophys. Cornelius Octavian Schwarze Jena [2022?] 1 Online-Ressource (XVII, 141 Seiten + Anhang) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 Dissertation Friedrich-Schiller-Universität Jena 2022 Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Zusammenfassungen in deutscher und englischer Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4041915-0 (DE-627)106216899 (DE-576)209047615 Neuseeland gnd s (DE-588)4334619-4 (DE-627)148298354 (DE-576)211350044 Forearc-Becken gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4384538-1 (DE-627)187467080 (DE-576)21188118X Submarine Gleitung gnd s (DE-588)4409345-7 (DE-627)198336772 (DE-576)21214555X Deformation Geologie gnd (DE-627) s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4194294-2 (DE-627)105220574 (DE-576)210093102 Tiefseeberg gnd s (DE-588)4463868-1 (DE-627)231348444 (DE-576)212701118 Tiefseegraben gnd s (DE-588)4064937-4 (DE-627)104297778 (DE-576)209155922 Wechselwirkung gnd (DE-627) Kukowski, Nina 1960- akademischer betreuerin (DE-588)17220092X (DE-627)697114465 (DE-576)133070980 dgs Schmitt, Axel Karl 1968- akademischer betreuerin (DE-588)121915506 (DE-627)705701522 (DE-576)292990308 dgs Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Schwarze, Cornelius, 1988 - Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) Jena, 2022 XVII, 141 Seiten (DE-627)1801047839 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 Langzeitarchivierung Resolving-System kostenfrei https://d-nb.info/1322364494/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://www.db-thueringen.de/receive/dbt_mods_00051941 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OLC-PHA 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_31 ISIL_DE-27 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_381 ISIL_DE-Ki130 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER 38.36 Tektonik (DE-627)106407147 38.41 Sedimentation (DE-627)106407090 38.19 Historische Geologie: Sonstiges (DE-627)106408232 BO 20 01 0084 4508104533 x 08-04-24 21 01 0046 4508121098 z 08-04-24 22 01 0018 4508137857 SUBolrd xu 08-04-24 23 01 0830 4508154522 olr-d x 08-04-24 30 01 0104 4508164072 z 08-04-24 31 01 0027 4130242407 z 09-05-22 40 01 0007 4508172032 xsn 08-04-24 60 01 0705 4508188567 OLRD z 08-04-24 63 01 3401 4508205364 ORD x 08-04-24 70 01 0089 4508213030 zdo 08-04-24 105 01 0841 4508358292 z 08-04-24 110 01 3110 4508222862 x 08-04-24 132 01 0959 4508232825 OLR-DISS x 08-04-24 151 01 0546 4508249728 OLR-ODISS z 08-04-24 161 01 0960 4508255671 ORD z 08-04-24 293 01 3293 4508289584 ORD z 08-04-24 370 01 4370 4508299407 x 08-04-24 381 01 4381 4569385168 z 21-08-24 2027 01 DE-105 4135924972 00 --%%-- Dn --%%-- --%%-- l01 18-05-22 2403 01 DE-LFER 4143595974 00 --%%-- --%%-- n --%%-- l01 07-06-22 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 01 0027 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 40 01 0007 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 381 01 4381 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 381 00 DE-Ki130 00 Seamount 381 00 DE-Ki130 00 Subduction 381 00 DE-Ki130 00 Landslide 381 00 DE-Ki130 00 Hikurangi Margin 381 00 DE-Ki130 00 New Zealand 381 00 DE-Ki130 00 Online publication 381 00 DE-Ki130 00 Dissertation 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 2027 01 DE-105 00 (DE-627)1298242568 DK 551.435.62 2027 01 DE-105 00 (DE-627)1294054791 DK 551.242.4 2027 01 DE-105 00 (DE-627)1297637046 DK 551.462.6 2027 01 DE-105 00 (DE-627)1293787280 DK 919.31 2027 01 DE-105 00 (DE-627)129278105X DK 378.245 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 2024-04-08 07:43:14 |
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urn:nbn:de:gbv:27-dbt-20220505-145014-009 urn (DE-627)1801169950 (DE-599)KXP1801169950 (OCoLC)1314887796 DE-627 ger DE-627 rda eng ger XA-DE-TH 551.136 DE-101 550 DE-101 38.36 bkl 38.41 bkl 38.19 bkl Schwarze, Cornelius 1988- verfasserin (DE-588)1256892106 (DE-627)1801046514 aut Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) von Dipl.-Geophys. Cornelius Octavian Schwarze Jena [2022?] 1 Online-Ressource (XVII, 141 Seiten + Anhang) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Volltext: PDF Literaturverzeichnis: Seite 119-135 Kumulative Dissertation, enthält Zeitschriftenaufsätze Tag der Verteidigung: 06.04.2022 Dissertation Friedrich-Schiller-Universität Jena 2022 Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. During the last decades, sample research has improved our knowledge of tectonics and sedimentation of a convergent margin as well as eruption history of backarc/arc volcanism. Parameters controlling tectonic erosion, sediment accretion, sediment architecture, and sediment instabilities of convergent margins are largely dependent on a multitude of geological conditions and have to be assessed individually for each case study. In this context, it is not only important to answer questions about the interaction of the overriding and subducting plates, but also about the temporal evolution of the continental margin and its response to changes in paleoclimatology. Studies undertaken in the framework of this doctoral project aim to contribute to answer the above developed questions by studying the sedimentation processes and stability of an accretionary ridge as well as the décollement at the Hikurangi Margin east off the North Island of New Zealand. The investigation area Rock Garden is an outermost sedimentary accretionary ridge in central Hikurangi Margin with an oversteep trenchward flank as a consequence of uplift above a subducting seamount. Studies presented in this thesis integrate high-resolution bathymetry and interface geometry of the subducting plate, high-resolution acoustic datasets with a wealth of data sets retrieved from drilled core material in order to address (1) the detachment strength and mechanical segmentation of the Hikurangi Margin, (2) the influence of seamount subduction and excess fluid pressure on slope failure, (3) the Quaternary marine tephrochronology of the frontal sediment accretionary ridge, and (4) patterns and cyclicity of Quaternary sediments at Rock Garden. Zusammenfassungen in deutscher und englischer Sprache Archivierung/Langzeitarchivierung gewährleistet XA-DE-TH pdager DE-27 Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4041915-0 (DE-627)106216899 (DE-576)209047615 Neuseeland gnd s (DE-588)4334619-4 (DE-627)148298354 (DE-576)211350044 Forearc-Becken gnd s (DE-588)4418304-5 (DE-627)213357410 (DE-576)212237373 Akkretionskeil gnd s (DE-588)4183899-3 (DE-627)105299286 (DE-576)210021926 Subduktion gnd s (DE-588)4384538-1 (DE-627)187467080 (DE-576)21188118X Submarine Gleitung gnd s (DE-588)4409345-7 (DE-627)198336772 (DE-576)21214555X Deformation Geologie gnd (DE-627) s (DE-588)4038316-7 (DE-627)106232916 (DE-576)209029463 Meeresgeologie gnd s (DE-588)4194294-2 (DE-627)105220574 (DE-576)210093102 Tiefseeberg gnd s (DE-588)4463868-1 (DE-627)231348444 (DE-576)212701118 Tiefseegraben gnd s (DE-588)4064937-4 (DE-627)104297778 (DE-576)209155922 Wechselwirkung gnd (DE-627) Kukowski, Nina 1960- akademischer betreuerin (DE-588)17220092X (DE-627)697114465 (DE-576)133070980 dgs Schmitt, Axel Karl 1968- akademischer betreuerin (DE-588)121915506 (DE-627)705701522 (DE-576)292990308 dgs Friedrich-Schiller-Universität Jena Grad-verleihende Institution (DE-588)36164-1 (DE-627)100833012 (DE-576)190344695 dgg Jena (DE-588)4028557-1 (DE-627)104814411 (DE-576)208977872 uvp Erscheint auch als Druck-Ausgabe Schwarze, Cornelius, 1988 - Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) Jena, 2022 XVII, 141 Seiten (DE-627)1801047839 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 Langzeitarchivierung Resolving-System kostenfrei https://d-nb.info/1322364494/34 Langzeitarchivierung Nationalbibliothek kostenfrei https://www.db-thueringen.de/receive/dbt_mods_00051941 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OLC-PHA 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_31 ISIL_DE-27 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_381 ISIL_DE-Ki130 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER 38.36 Tektonik (DE-627)106407147 38.41 Sedimentation (DE-627)106407090 38.19 Historische Geologie: Sonstiges (DE-627)106408232 BO 20 01 0084 4508104533 x 08-04-24 21 01 0046 4508121098 z 08-04-24 22 01 0018 4508137857 SUBolrd xu 08-04-24 23 01 0830 4508154522 olr-d x 08-04-24 30 01 0104 4508164072 z 08-04-24 31 01 0027 4130242407 z 09-05-22 40 01 0007 4508172032 xsn 08-04-24 60 01 0705 4508188567 OLRD z 08-04-24 63 01 3401 4508205364 ORD x 08-04-24 70 01 0089 4508213030 zdo 08-04-24 105 01 0841 4508358292 z 08-04-24 110 01 3110 4508222862 x 08-04-24 132 01 0959 4508232825 OLR-DISS x 08-04-24 151 01 0546 4508249728 OLR-ODISS z 08-04-24 161 01 0960 4508255671 ORD z 08-04-24 293 01 3293 4508289584 ORD z 08-04-24 370 01 4370 4508299407 x 08-04-24 381 01 4381 4569385168 z 21-08-24 2027 01 DE-105 4135924972 00 --%%-- Dn --%%-- --%%-- l01 18-05-22 2403 01 DE-LFER 4143595974 00 --%%-- --%%-- n --%%-- l01 07-06-22 20 01 0084 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 21 01 0046 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 22 01 0018 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 23 01 0830 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 30 01 0104 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 01 0027 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 40 01 0007 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 60 01 0705 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 63 01 3401 E-Book https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 LF 70 01 0089 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 105 01 0841 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 110 01 3110 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 132 01 0959 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 151 01 0546 Volltext https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 161 01 0960 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 293 01 3293 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 370 01 4370 https://nbn-resolving.de/urn:nbn:de:gbv:27-dbt-20220505-145014-009 381 01 4381 https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 2403 01 DE-LFER https://nbn-resolving.org/urn:nbn:de:gbv:27-dbt-20220505-145014-009 31 00 DE-27 00 Universitätsbibliographie Jena 31 00 DE-27 01 Chemisch-Geowissenschaftliche Fakultät 381 00 DE-Ki130 00 Seamount 381 00 DE-Ki130 00 Subduction 381 00 DE-Ki130 00 Landslide 381 00 DE-Ki130 00 Hikurangi Margin 381 00 DE-Ki130 00 New Zealand 381 00 DE-Ki130 00 Online publication 381 00 DE-Ki130 00 Dissertation 2027 01 DE-105 00 s ebook 60 01 0705 10 ho 2027 01 DE-105 00 (DE-627)1298242568 DK 551.435.62 2027 01 DE-105 00 (DE-627)1294054791 DK 551.242.4 2027 01 DE-105 00 (DE-627)1297637046 DK 551.462.6 2027 01 DE-105 00 (DE-627)1293787280 DK 919.31 2027 01 DE-105 00 (DE-627)129278105X DK 378.245 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 2024-04-08 07:43:14 |
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Schwarze, Cornelius @@aut@@ Kukowski, Nina @@dgs@@ Schmitt, Axel Karl @@dgs@@ |
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ddc 551.136 ddc 550 bkl 38.36 bkl 38.41 bkl 38.19 gnd Neuseeland gnd Forearc-Becken gnd Akkretionskeil gnd Subduktion gnd Submarine Gleitung gnd Deformation gnd Meeresgeologie gnd Tiefseeberg gnd Tiefseegraben gnd Wechselwirkung 31 Universitätsbibliographie Jena 31 Chemisch-Geowissenschaftliche Fakultät 381 Seamount 381 Subduction 381 Landslide 381 Hikurangi Margin 381 New Zealand 381 Online publication 381 Dissertation 2027 ebook |
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Outer forearc architecture and submarine landslides related to seamount subduction at the Hikurangi Margin (offshore New Zealand) |
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Schwarze, Cornelius Octavian Schwarze, C. Schwarze, Cornelius O. Schwarze, Cornelius Hochschulschrift New Zealand Aetearo New Zealand (Dominion) Dominion of New Zealand Nouvelle-Zélande Aotearoa Neuseeland Inselbogen-Außenbecken Vorderbogenbecken Forearc-Becken Akkretionskeil Subduktionszone Subduktion Unterseeische Gleitung Submarine Rutschung Unterseeische Rutschung Submarine Gleitung Strain Deformation <Geologie> Submarine Geologie Meeresboden / Geologie Meeresgeologie Tiefseekuppe Seamount Sea mount Tiefseeberg Tiefseegesenke Tiefseerinne Tiefseegraben Wechselwirkungen Interaktion <Naturwissenschaft> Wechselwirkung Kukowski, Nina Schmitt, A. K. Schmitt, Axel K. Schmitt, Axel Schmitt, Axel Karl Schiller-Universität Jena University (Jena) University of Jena Universitet Imeni Fridricha Šillera (Jena) Schiller University (Jena) Universität Jena Friedrich-Schiller-Universität Jena. Rektor Friedrich Schiller University (Jena) Gosudarstvennyj Universitet Imeni Fridricha Šillera (Jena) Universidad Friedrich Schiller FSU Jena Universitas Litterarum Jenensis Jenskij Gosudarstvennyj Universitet Imeni Fridricha Šillera Universitas Litterarum Ienensis Alma Mater Jenensis Friedrich-Schiller-Universität Jena Jhena Ihena Stadt Jena City of Jena Iena Iéna Jena (Lichtstadt) Jehna Giena Gena Jena |
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Schwarze, Cornelius Octavian Schwarze, C. Schwarze, Cornelius O. Schwarze, Cornelius Hochschulschrift New Zealand Aetearo New Zealand (Dominion) Dominion of New Zealand Nouvelle-Zélande Aotearoa Neuseeland Inselbogen-Außenbecken Vorderbogenbecken Forearc-Becken Akkretionskeil Subduktionszone Subduktion Unterseeische Gleitung Submarine Rutschung Unterseeische Rutschung Submarine Gleitung Strain Deformation <Geologie> Submarine Geologie Meeresboden / Geologie Meeresgeologie Tiefseekuppe Seamount Sea mount Tiefseeberg Tiefseegesenke Tiefseerinne Tiefseegraben Wechselwirkungen Interaktion <Naturwissenschaft> Wechselwirkung Kukowski, Nina Schmitt, A. K. Schmitt, Axel K. Schmitt, Axel Schmitt, Axel Karl Schiller-Universität Jena University (Jena) University of Jena Universitet Imeni Fridricha Šillera (Jena) Schiller University (Jena) Universität Jena Friedrich-Schiller-Universität Jena. Rektor Friedrich Schiller University (Jena) Gosudarstvennyj Universitet Imeni Fridricha Šillera (Jena) Universidad Friedrich Schiller FSU Jena Universitas Litterarum Jenensis Jenskij Gosudarstvennyj Universitet Imeni Fridricha Šillera Universitas Litterarum Ienensis Alma Mater Jenensis Friedrich-Schiller-Universität Jena Jhena Ihena Stadt Jena City of Jena Iena Iéna Jena (Lichtstadt) Jehna Giena Gena Jena |
GND_txtF_mv |
Schwarze, Cornelius Octavian Schwarze, C. Schwarze, Cornelius O. Schwarze, Cornelius Hochschulschrift New Zealand Aetearo New Zealand (Dominion) Dominion of New Zealand Nouvelle-Zélande Aotearoa Neuseeland Inselbogen-Außenbecken Vorderbogenbecken Forearc-Becken Akkretionskeil Subduktionszone Subduktion Unterseeische Gleitung Submarine Rutschung Unterseeische Rutschung Submarine Gleitung Strain Deformation <Geologie> Submarine Geologie Meeresboden / Geologie Meeresgeologie Tiefseekuppe Seamount Sea mount Tiefseeberg Tiefseegesenke Tiefseerinne Tiefseegraben Wechselwirkungen Interaktion <Naturwissenschaft> Wechselwirkung Kukowski, Nina Schmitt, A. K. Schmitt, Axel K. Schmitt, Axel Schmitt, Axel Karl Schiller-Universität Jena University (Jena) University of Jena Universitet Imeni Fridricha Šillera (Jena) Schiller University (Jena) Universität Jena Friedrich-Schiller-Universität Jena. Rektor Friedrich Schiller University (Jena) Gosudarstvennyj Universitet Imeni Fridricha Šillera (Jena) Universidad Friedrich Schiller FSU Jena Universitas Litterarum Jenensis Jenskij Gosudarstvennyj Universitet Imeni Fridricha Šillera Universitas Litterarum Ienensis Alma Mater Jenensis Friedrich-Schiller-Universität Jena Jhena Ihena Stadt Jena City of Jena Iena Iéna Jena (Lichtstadt) Jehna Giena Gena Jena |
callnumber-a |
Dn |
up_date |
2024-08-22T04:53:22.750Z |
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1808062116270178304 |
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Cornelius Octavian Schwarze</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Jena</subfield><subfield code="c">[2022?]</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (XVII, 141 Seiten + Anhang)</subfield><subfield code="b">Illustrationen, Diagramme</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="500" ind1=" " ind2=" "><subfield code="a">Volltext: PDF</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Literaturverzeichnis: Seite 119-135</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Kumulative Dissertation, enthält Zeitschriftenaufsätze</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">Tag der Verteidigung: 06.04.2022</subfield></datafield><datafield tag="502" ind1=" " ind2=" "><subfield code="b">Dissertation</subfield><subfield code="c">Friedrich-Schiller-Universität Jena</subfield><subfield code="d">2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Sedimentation processes and tectonic mechanisms at the outer forearc of convergent margins are a subject of intense research, mainly owing to the inherent geological hazardous consequences associated with volcanism, seismic shaking, and gravitational mass movement. 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