Structural reorganization of the India-Arabia strike-slip plate boundary (Owen Fracture Zone; NW Indian Ocean) 2.4 million years ago
Autor: | Marc Fournier, Matthias Delescluse, Mathieu Rodriguez, Nicolas Chamot-Rooke, Philippe Huchon |
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Přispěvatelé: | Laboratoire de géologie de l'ENS (LGE), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris), Institut des Sciences de la Terre de Paris (iSTeP), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Joao C. Duarte, Laboratoire de géologie de l'ENS (LGENS), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS) |
Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
fracture zone
Transform fault Pull apart basin horsetail [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Fracture zone Present day Strike-slip tectonics Cretaceous pull-apart basin Paleontology Plate tectonics Sinistral and dextral [SDU]Sciences of the Universe [physics] 14. Life underwater Indian Ocean Geology |
Zdroj: | Transform Plate Boundaries and Fracture Zones Joao C. Duarte. Transform Plate Boundaries and Fracture Zones, Elsevier, pp.146-155, 2018, ⟨10.1016/B978-0-12-812064-4.00007-4⟩ Joao C. Duarte. Transform Plate Boundaries and Fracture Zones, Elsevier, pp.146-155, 2019, ⟨10.1016/B978-0-12-812064-4.00007-4⟩ |
Popis: | International audience; The Owen Fracture Zone (OFZ) is the present-day, 800-km-long dextral India Arabia plate boundary, with conspicuous pull-apart basins at stepover areas and at its terminations. We summarize geological evidence documenting the age of formation of the OFZ, based on detailed analysis of geophysical and drilling data in the vicinity of the main pull-apart basins. Although India-Arabia motion started in the Late Cretaceous, we show that the present-day OFZ is a young structure formed at 2.4 Ma. This last structural reorganization of the India-Arabia plate boundary is unrelated to any well-documented kinematic change, leaving questions over its driver. |
Databáze: | OpenAIRE |
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