Neogene strike-slip faulting in Sakhalin and the Japan Sea opening
Laurent Jolivet est Professeur à l'Université d'Orléans au 1er Septembre 2009 International audience We describe structural data from a 2000 km N-S dextral strike-slip zone extending from northern Sakhalin to the southeast corner of the Japan Sea. Satellite images, field data, and focal me...
Published in: | Journal of Geophysical Research: Solid Earth |
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Main Authors: | , , , , |
Other Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
1994
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Online Access: | https://hal-insu.archives-ouvertes.fr/insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734/document https://hal-insu.archives-ouvertes.fr/insu-00726734/file/93JB02026.pdf https://doi.org/10.1029/93JB02026 |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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English |
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[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes Fournier, Marc Jolivet, Laurent Huchon, Philippe Sergeyev, Konstantin F. Oscorbin, Leonid Neogene strike-slip faulting in Sakhalin and the Japan Sea opening |
topic_facet |
[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes |
description |
Laurent Jolivet est Professeur à l'Université d'Orléans au 1er Septembre 2009 International audience We describe structural data from a 2000 km N-S dextral strike-slip zone extending from northern Sakhalin to the southeast corner of the Japan Sea. Satellite images, field data, and focal mechanisms of earthquakes in Sakhalin are included in the interpretation. Since Miocene time the deformation in Sakhalin has been taken up by N-S dextral strike-slip faults with a reverse component and associated en e'chelon folds. Narrow en échelon Neogene basins were formed along strike-sup faults and were later folded in a second stage of deformation. We propose a model of basin formation along extension al faults delimitating dominos between two major strike-slip faults, and subsequent counterclockwise rotation of the dominos in a dextral transpressional regime, basins becoming progressively oblique to the direction of maximum horizontal compression and undergoing shortening. The association of both dextral and compressional focal mechanisms of earthquakes indicates that the same transpressional regime still prevails today in Sakhalin. We present fault set measurements undertaken in Noto Peninsula and Yatsuo Basin at the southern end of the Sakhalin-East Japan Sea strike-slip zone. Early and middle Miocene formations recorded the same transtensional regime as observed along the west coast of NE Honshu. During the early and middle Miocene the strike-slip regime was transpressional to the north in Sakhalin and Hokkaido, and transtensional to the south along the west coast of NE Honshu as far as Noto Peninsula and Yatsuo basin. Dextral motion accommodated the opening of the Japan Sea as a pull-apart basin, with the Tsushima fault to the west. The opening of the Japan Sea ceased at the end of the middle Miocene when transtension started to change to E-W compression in the Japan arc. Subduction of the Japan Sea lithosphere under the Japan arc started 1.8 Ma ago. The evolution of the stress regime from transtensional to ... |
author2 |
Institut des Sciences de la Terre de Paris (iSTeP) Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géologie (URA 316) École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL) Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Institute of Marine Geology and Geophysics FEB RAS (IMGG) Far Eastern Branch of the Russian Academy of Sciences (FEB RAS) |
format |
Article in Journal/Newspaper |
author |
Fournier, Marc Jolivet, Laurent Huchon, Philippe Sergeyev, Konstantin F. Oscorbin, Leonid |
author_facet |
Fournier, Marc Jolivet, Laurent Huchon, Philippe Sergeyev, Konstantin F. Oscorbin, Leonid |
author_sort |
Fournier, Marc |
title |
Neogene strike-slip faulting in Sakhalin and the Japan Sea opening |
title_short |
Neogene strike-slip faulting in Sakhalin and the Japan Sea opening |
title_full |
Neogene strike-slip faulting in Sakhalin and the Japan Sea opening |
title_fullStr |
Neogene strike-slip faulting in Sakhalin and the Japan Sea opening |
title_full_unstemmed |
Neogene strike-slip faulting in Sakhalin and the Japan Sea opening |
title_sort |
neogene strike-slip faulting in sakhalin and the japan sea opening |
publisher |
HAL CCSD |
publishDate |
1994 |
url |
https://hal-insu.archives-ouvertes.fr/insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734/document https://hal-insu.archives-ouvertes.fr/insu-00726734/file/93JB02026.pdf https://doi.org/10.1029/93JB02026 |
long_lat |
ENVELOPE(-60.811,-60.811,-62.471,-62.471) |
geographic |
Noto |
geographic_facet |
Noto |
genre |
Sakhalin |
genre_facet |
Sakhalin |
op_source |
ISSN: 2169-9313 EISSN: 2169-9356 Journal of Geophysical Research : Solid Earth https://hal-insu.archives-ouvertes.fr/insu-00726734 Journal of Geophysical Research : Solid Earth, American Geophysical Union, 1994, 99 (B2), pp.2701-2725. ⟨10.1029/93JB02026⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1029/93JB02026 insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734/document https://hal-insu.archives-ouvertes.fr/insu-00726734/file/93JB02026.pdf doi:10.1029/93JB02026 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/93JB02026 |
container_title |
Journal of Geophysical Research: Solid Earth |
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99 |
container_issue |
B2 |
container_start_page |
2701 |
op_container_end_page |
2725 |
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1766181039422570496 |
spelling |
ftccsdartic:oai:HAL:insu-00726734v1 2023-05-15T18:08:43+02:00 Neogene strike-slip faulting in Sakhalin and the Japan Sea opening Fournier, Marc Jolivet, Laurent Huchon, Philippe Sergeyev, Konstantin F. Oscorbin, Leonid Institut des Sciences de la Terre de Paris (iSTeP) Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géologie (URA 316) École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL) Institut des Sciences de la Terre d'Orléans (ISTO) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Institute of Marine Geology and Geophysics FEB RAS (IMGG) Far Eastern Branch of the Russian Academy of Sciences (FEB RAS) 1994 https://hal-insu.archives-ouvertes.fr/insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734/document https://hal-insu.archives-ouvertes.fr/insu-00726734/file/93JB02026.pdf https://doi.org/10.1029/93JB02026 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/93JB02026 insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734 https://hal-insu.archives-ouvertes.fr/insu-00726734/document https://hal-insu.archives-ouvertes.fr/insu-00726734/file/93JB02026.pdf doi:10.1029/93JB02026 info:eu-repo/semantics/OpenAccess ISSN: 2169-9313 EISSN: 2169-9356 Journal of Geophysical Research : Solid Earth https://hal-insu.archives-ouvertes.fr/insu-00726734 Journal of Geophysical Research : Solid Earth, American Geophysical Union, 1994, 99 (B2), pp.2701-2725. ⟨10.1029/93JB02026⟩ [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 1994 ftccsdartic https://doi.org/10.1029/93JB02026 2021-11-21T04:03:29Z Laurent Jolivet est Professeur à l'Université d'Orléans au 1er Septembre 2009 International audience We describe structural data from a 2000 km N-S dextral strike-slip zone extending from northern Sakhalin to the southeast corner of the Japan Sea. Satellite images, field data, and focal mechanisms of earthquakes in Sakhalin are included in the interpretation. Since Miocene time the deformation in Sakhalin has been taken up by N-S dextral strike-slip faults with a reverse component and associated en e'chelon folds. Narrow en échelon Neogene basins were formed along strike-sup faults and were later folded in a second stage of deformation. We propose a model of basin formation along extension al faults delimitating dominos between two major strike-slip faults, and subsequent counterclockwise rotation of the dominos in a dextral transpressional regime, basins becoming progressively oblique to the direction of maximum horizontal compression and undergoing shortening. The association of both dextral and compressional focal mechanisms of earthquakes indicates that the same transpressional regime still prevails today in Sakhalin. We present fault set measurements undertaken in Noto Peninsula and Yatsuo Basin at the southern end of the Sakhalin-East Japan Sea strike-slip zone. Early and middle Miocene formations recorded the same transtensional regime as observed along the west coast of NE Honshu. During the early and middle Miocene the strike-slip regime was transpressional to the north in Sakhalin and Hokkaido, and transtensional to the south along the west coast of NE Honshu as far as Noto Peninsula and Yatsuo basin. Dextral motion accommodated the opening of the Japan Sea as a pull-apart basin, with the Tsushima fault to the west. The opening of the Japan Sea ceased at the end of the middle Miocene when transtension started to change to E-W compression in the Japan arc. Subduction of the Japan Sea lithosphere under the Japan arc started 1.8 Ma ago. The evolution of the stress regime from transtensional to ... Article in Journal/Newspaper Sakhalin Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Noto ENVELOPE(-60.811,-60.811,-62.471,-62.471) Journal of Geophysical Research: Solid Earth 99 B2 2701 2725 |