Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage
International audience At the NW corner of the Pacific region, just south of the Kamchatsky Peninsula, the northern tip of Pacific plate subduction and associated volcanic arc interacts with the western end of the Aleutian-Komandorsky dextral transform plate boundary and associated arc. Study of bot...
Published in: | Tectonics |
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Main Authors: | , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2013
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Subjects: | |
Online Access: | https://hal-insu.archives-ouvertes.fr/insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284/document https://hal-insu.archives-ouvertes.fr/insu-00852284/file/tect.20051.pdf https://doi.org/10.1002/tect.20051 |
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Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
collision marine terrace sequence drainage active tectonics geomorphometry morphotectonics Kamchatsky peninsula Kamchatka [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
collision marine terrace sequence drainage active tectonics geomorphometry morphotectonics Kamchatsky peninsula Kamchatka [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes Pedoja, Kevin Authemayou, Christine Pinegina, T. K. Bourgeois, J. Nexer, M. Delcaillau, Bernard Regard, Vincent Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage |
topic_facet |
collision marine terrace sequence drainage active tectonics geomorphometry morphotectonics Kamchatsky peninsula Kamchatka [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience At the NW corner of the Pacific region, just south of the Kamchatsky Peninsula, the northern tip of Pacific plate subduction and associated volcanic arc interacts with the western end of the Aleutian-Komandorsky dextral transform plate boundary and associated arc. Study of both Holocene and Pleistocene sequences of uplifted marine terraces and also of fluvial drainage patterns on the Kamchatsky Peninsula allows us to highlight active tectonics produced by complex plate interaction. Our results show that the central - eastern coast of the peninsula is currently divided into four different zones consisting in uplifted blocks associated with various uplift rates in front of a fold and thrust zone to the west. Our main tectonic benchmark--the altitude of the shoreline correlated to last interglacial maximum (MIS 5e)--yields Late Pleistocene uplift rates ranging from 0.2 to 2.74 mm/yr. One of the main active faults bounding the coastal blocks is dextral and is interpreted as a prolongation of an offshore fault of the Aleutian-Komandorsky dextral transform plate boundary. We suggest that structures on the Kamchatsky Peninsula accommodate a part of the transform motion, but that mainly the arc-continent collision of the Aleutian arc against Kamchatka produces a "bulldozer" effect on the Kamchatsky Peninsula. |
author2 |
Morphodynamique Continentale et Côtière (M2C) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Institute of Volcanology and Seismology of the RAS Far Eastern Branch of the Russian Academy of Sciences (FEB RAS) Department of Earth and Space Sciences Seattle University of Washington Seattle Laboratoire des Mécanismes et Transfert en Géologie (LMTG) Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) EAR-0125787 |
format |
Article in Journal/Newspaper |
author |
Pedoja, Kevin Authemayou, Christine Pinegina, T. K. Bourgeois, J. Nexer, M. Delcaillau, Bernard Regard, Vincent |
author_facet |
Pedoja, Kevin Authemayou, Christine Pinegina, T. K. Bourgeois, J. Nexer, M. Delcaillau, Bernard Regard, Vincent |
author_sort |
Pedoja, Kevin |
title |
Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage |
title_short |
Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage |
title_full |
Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage |
title_fullStr |
Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage |
title_full_unstemmed |
Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage |
title_sort |
arc-continent collision" of the aleutian-komandorsky arc into kamchatka: insight into quaternary tectonic segmentation through pleistocene marine terraces and morphometric analysis of fluvial drainage |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal-insu.archives-ouvertes.fr/insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284/document https://hal-insu.archives-ouvertes.fr/insu-00852284/file/tect.20051.pdf https://doi.org/10.1002/tect.20051 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
ISSN: 0278-7407 EISSN: 1944-9194 Tectonics https://hal-insu.archives-ouvertes.fr/insu-00852284 Tectonics, 2013, 32 (4), pp.827-842. ⟨10.1002/tect.20051⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/tect.20051 insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284/document https://hal-insu.archives-ouvertes.fr/insu-00852284/file/tect.20051.pdf doi:10.1002/tect.20051 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1002/tect.20051 |
container_title |
Tectonics |
container_start_page |
n/a |
op_container_end_page |
n/a |
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1766050875838562304 |
spelling |
ftunivnantes:oai:HAL:insu-00852284v1 2023-05-15T16:58:47+02:00 Arc-continent collision" of the Aleutian-Komandorsky arc into Kamchatka: insight into Quaternary tectonic segmentation through Pleistocene marine terraces and morphometric analysis of fluvial drainage Pedoja, Kevin Authemayou, Christine Pinegina, T. K. Bourgeois, J. Nexer, M. Delcaillau, Bernard Regard, Vincent Morphodynamique Continentale et Côtière (M2C) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Institute of Volcanology and Seismology of the RAS Far Eastern Branch of the Russian Academy of Sciences (FEB RAS) Department of Earth and Space Sciences Seattle University of Washington Seattle Laboratoire des Mécanismes et Transfert en Géologie (LMTG) Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS) EAR-0125787 2013-08-20 https://hal-insu.archives-ouvertes.fr/insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284/document https://hal-insu.archives-ouvertes.fr/insu-00852284/file/tect.20051.pdf https://doi.org/10.1002/tect.20051 en eng HAL CCSD American Geophysical Union (AGU) info:eu-repo/semantics/altIdentifier/doi/10.1002/tect.20051 insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284 https://hal-insu.archives-ouvertes.fr/insu-00852284/document https://hal-insu.archives-ouvertes.fr/insu-00852284/file/tect.20051.pdf doi:10.1002/tect.20051 info:eu-repo/semantics/OpenAccess ISSN: 0278-7407 EISSN: 1944-9194 Tectonics https://hal-insu.archives-ouvertes.fr/insu-00852284 Tectonics, 2013, 32 (4), pp.827-842. ⟨10.1002/tect.20051⟩ collision marine terrace sequence drainage active tectonics geomorphometry morphotectonics Kamchatsky peninsula Kamchatka [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2013 ftunivnantes https://doi.org/10.1002/tect.20051 2023-02-22T03:49:40Z International audience At the NW corner of the Pacific region, just south of the Kamchatsky Peninsula, the northern tip of Pacific plate subduction and associated volcanic arc interacts with the western end of the Aleutian-Komandorsky dextral transform plate boundary and associated arc. Study of both Holocene and Pleistocene sequences of uplifted marine terraces and also of fluvial drainage patterns on the Kamchatsky Peninsula allows us to highlight active tectonics produced by complex plate interaction. Our results show that the central - eastern coast of the peninsula is currently divided into four different zones consisting in uplifted blocks associated with various uplift rates in front of a fold and thrust zone to the west. Our main tectonic benchmark--the altitude of the shoreline correlated to last interglacial maximum (MIS 5e)--yields Late Pleistocene uplift rates ranging from 0.2 to 2.74 mm/yr. One of the main active faults bounding the coastal blocks is dextral and is interpreted as a prolongation of an offshore fault of the Aleutian-Komandorsky dextral transform plate boundary. We suggest that structures on the Kamchatsky Peninsula accommodate a part of the transform motion, but that mainly the arc-continent collision of the Aleutian arc against Kamchatka produces a "bulldozer" effect on the Kamchatsky Peninsula. Article in Journal/Newspaper Kamchatka Université de Nantes: HAL-UNIV-NANTES Pacific Tectonics n/a n/a |