Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study
International audience The Tunka Basin is a broad, emerging basin situated between the Baikal Lake to the east and the the Hövsgöl Lake to the west. The basin is bounded to the north and to the south by the Tunka and the Khamar-Daban mountain ranges, respectively. The Tunka normal fault, located at...
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ftccsdartic:oai:HAL:hal-02978189v1 2023-05-15T17:57:56+02:00 Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study Arzhannikova, Anastasia Ritz, Jean-François Larroque, Christophe Antoine, Pierre Arzhannikov, Sergey Chebotarev, Aleksei Stéphan, Jean-François Marc Massault, M. Michelot, Jean-Luc Institute of the Earth's Crust (IEC) Siberian Branch of the Russian Academy of Sciences (SB RAS) Géosciences Montpellier Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Université des Antilles (UA) Géoazur (GEOAZUR 7329) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Sud ) Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Géosciences Paris Saclay (GEOPS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) 2020-10-24 https://hal.archives-ouvertes.fr/hal-02978189 https://doi.org/10.1016/j.jseaes.2020.104569 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jseaes.2020.104569 hal-02978189 https://hal.archives-ouvertes.fr/hal-02978189 doi:10.1016/j.jseaes.2020.104569 ISSN: 1367-9120 Journal of Asian Earth Sciences https://hal.archives-ouvertes.fr/hal-02978189 Journal of Asian Earth Sciences, Elsevier, 2020, 204, pp.104569. ⟨10.1016/j.jseaes.2020.104569⟩ [SDE]Environmental Sciences [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2020 ftccsdartic https://doi.org/10.1016/j.jseaes.2020.104569 2020-12-23T22:51:39Z International audience The Tunka Basin is a broad, emerging basin situated between the Baikal Lake to the east and the the Hövsgöl Lake to the west. The basin is bounded to the north and to the south by the Tunka and the Khamar-Daban mountain ranges, respectively. The Tunka normal fault, located at the southern foothills of the Tunka mountain range, is the main structure that controlled the development of the Tunka Basin during the Neogene. Paleoearthquake-surface ruptures attest of its present activity; and show that its western and eastern terminations are undergoing a tectonic inversion characterized by left-lateral-reverse deformations. The southern edge of the Tunka Basin is classically interpreted as being tectonically controlled. In this paper, we present the results of a geomorphological and stratigraphic analysis within its southwestern and southeastern parts suggesting that there is no active fault affecting the foothills of the Khamar-Daban mountain range. The different features observed in the Quaternary deposits are interpreted to be the result of periglacial processes induced by alternating episodes of permafrost aggradation and degradation during the Holocene. Our study concludes that the Khamar-Daban Range and the Tunka Basin are uplifting together, and that the Tunka and Mondy faults are the two main triggers of regional earthquakes. Article in Journal/Newspaper permafrost Siberia Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Journal of Asian Earth Sciences 204 104569 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDE]Environmental Sciences [SDU]Sciences of the Universe [physics] |
spellingShingle |
[SDE]Environmental Sciences [SDU]Sciences of the Universe [physics] Arzhannikova, Anastasia Ritz, Jean-François Larroque, Christophe Antoine, Pierre Arzhannikov, Sergey Chebotarev, Aleksei Stéphan, Jean-François Marc Massault, M. Michelot, Jean-Luc Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study |
topic_facet |
[SDE]Environmental Sciences [SDU]Sciences of the Universe [physics] |
description |
International audience The Tunka Basin is a broad, emerging basin situated between the Baikal Lake to the east and the the Hövsgöl Lake to the west. The basin is bounded to the north and to the south by the Tunka and the Khamar-Daban mountain ranges, respectively. The Tunka normal fault, located at the southern foothills of the Tunka mountain range, is the main structure that controlled the development of the Tunka Basin during the Neogene. Paleoearthquake-surface ruptures attest of its present activity; and show that its western and eastern terminations are undergoing a tectonic inversion characterized by left-lateral-reverse deformations. The southern edge of the Tunka Basin is classically interpreted as being tectonically controlled. In this paper, we present the results of a geomorphological and stratigraphic analysis within its southwestern and southeastern parts suggesting that there is no active fault affecting the foothills of the Khamar-Daban mountain range. The different features observed in the Quaternary deposits are interpreted to be the result of periglacial processes induced by alternating episodes of permafrost aggradation and degradation during the Holocene. Our study concludes that the Khamar-Daban Range and the Tunka Basin are uplifting together, and that the Tunka and Mondy faults are the two main triggers of regional earthquakes. |
author2 |
Institute of the Earth's Crust (IEC) Siberian Branch of the Russian Academy of Sciences (SB RAS) Géosciences Montpellier Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)-Université des Antilles (UA) Géoazur (GEOAZUR 7329) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Université Côte d'Azur (UCA)-COMUE Université Côte d'Azur (2015 - 2019) (COMUE UCA)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD France-Sud ) Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Géosciences Paris Saclay (GEOPS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Arzhannikova, Anastasia Ritz, Jean-François Larroque, Christophe Antoine, Pierre Arzhannikov, Sergey Chebotarev, Aleksei Stéphan, Jean-François Marc Massault, M. Michelot, Jean-Luc |
author_facet |
Arzhannikova, Anastasia Ritz, Jean-François Larroque, Christophe Antoine, Pierre Arzhannikov, Sergey Chebotarev, Aleksei Stéphan, Jean-François Marc Massault, M. Michelot, Jean-Luc |
author_sort |
Arzhannikova, Anastasia |
title |
Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study |
title_short |
Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study |
title_full |
Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study |
title_fullStr |
Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study |
title_full_unstemmed |
Cryoturbation versus tectonic deformation along the southern edge of the Tunka Basin (Baikal Rift System), Siberia: New insights from an integrated morphotectonic and stratigraphic study |
title_sort |
cryoturbation versus tectonic deformation along the southern edge of the tunka basin (baikal rift system), siberia: new insights from an integrated morphotectonic and stratigraphic study |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.archives-ouvertes.fr/hal-02978189 https://doi.org/10.1016/j.jseaes.2020.104569 |
genre |
permafrost Siberia |
genre_facet |
permafrost Siberia |
op_source |
ISSN: 1367-9120 Journal of Asian Earth Sciences https://hal.archives-ouvertes.fr/hal-02978189 Journal of Asian Earth Sciences, Elsevier, 2020, 204, pp.104569. ⟨10.1016/j.jseaes.2020.104569⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.jseaes.2020.104569 hal-02978189 https://hal.archives-ouvertes.fr/hal-02978189 doi:10.1016/j.jseaes.2020.104569 |
op_doi |
https://doi.org/10.1016/j.jseaes.2020.104569 |
container_title |
Journal of Asian Earth Sciences |
container_volume |
204 |
container_start_page |
104569 |
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1766166444865748992 |