Zobrazeno 1 - 10
of 94
pro vyhledávání: '"Philippe Huchon"'
Autor:
Alexandre Janin, Nicolas Chamot‐Rooke, Matthias Delescluse, Marc Fournier, Jean‐Arthur Olive, Alain Rabaute, Philippe Huchon, Jérôme Dyment, Christophe Vigny, Mathieu Rodriguez
Publikováno v:
Tectonics (0278-7407) (American Geophysical Union (AGU)), 2023-05, Vol. 42, N. 5, P. e2023TC007747 (35p.)
The Owen Transform Fault (OTF) connecting the Sheba and the Carlsberg spreading ridges in the Indian Ocean currently forms the active plate boundary between India and Somalia plates. This 330-km-long transform fault is by far the longest transform fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9e7473501617812cb18e31626e0ef4e0
https://archimer.ifremer.fr/doc/00835/94691/
https://archimer.ifremer.fr/doc/00835/94691/
Autor:
Alain Rabaute, Marc Fournier, Mathieu Rodriguez, Nicolas Chamot-Rooke, Jérôme Dyment, Alexandre Janin, Christophe Vigny, Matthias Delescluse, Philippe Huchon, Jean-Arthur Olive
The Owen oceanic transform fault is a 300-km long linear structure connecting the Carlsberg and Sheba spreading centers in the northwest Indian Ocean. It presently forms with the Carlsberg ridge the active plate boundary between India and Somalia. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a592a36b65bf750244af0303b79e2f57
https://doi.org/10.5194/egusphere-egu21-3285
https://doi.org/10.5194/egusphere-egu21-3285
Autor:
Alexandre Janin, Mathieu Rodriguez, Nicolas Chamot-Rooke, Alain Rabaute, Matthias Delescluse, Jérôme Dyment, Marc Fournier, Philippe Huchon, Jean-Arthur Olive, Christophe Vigny
The Owen transform fault in the northwest Indian Ocean is a >300 km-long active structure that constitutes the active plate boundary between Somalia and India. The first-order fault geometry was reached in the Early Miocene when the Carlsberg Ridge p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8d38376e9472b263dd080dd5e911daa
https://doi.org/10.5194/egusphere-egu2020-7974
https://doi.org/10.5194/egusphere-egu2020-7974
Autor:
Marc Fournier, Mathieu Rodriguez, Philippe Huchon, Jean-Arthur Olive, Christophe Vigny, Jérôme Dyment, Matthias Delescluse, Alain Rabaute, Nicolas Chamot-Rooke, Alexandre Janin
A sizeable portion of oceanic lithosphere has been produced at the Carlsberg Ridge, one of the three major ridge branches that shaped the Indian Ocean. Accretion started in the Paleocene with the ultra-fast widening of the Arabian Sea to the North an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7339e9b8b0b113f3403e3afe46f7bf88
https://doi.org/10.5194/egusphere-egu2020-8997
https://doi.org/10.5194/egusphere-egu2020-8997
Publikováno v:
Tectonics
Tectonics, American Geophysical Union (AGU), 2018, 37 (5), pp.1552-1575. ⟨10.1029/2017TC004687⟩
Tectonics (0278-7407) (Amer Geophysical Union), 2018-05, Vol. 37, N. 5, P. 1552-1575
Tectonics, 2018, 37 (5), pp.1552-1575. ⟨10.1029/2017TC004687⟩
Tectonics, American Geophysical Union (AGU), 2018, 37 (5), pp.1552-1575. ⟨10.1029/2017TC004687⟩
Tectonics (0278-7407) (Amer Geophysical Union), 2018-05, Vol. 37, N. 5, P. 1552-1575
Tectonics, 2018, 37 (5), pp.1552-1575. ⟨10.1029/2017TC004687⟩
International audience; The Aden-Owen-Carlsberg triple junction is the place where Arabia, Somalia, and India meet in the Arabian Sea (NW Indian Ocean). Here we present a new seismic data set crossing a key structure of the triple junction, namely, t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::af35752fe38f94405914e2a08da520a3
https://hal.archives-ouvertes.fr/hal-02323917
https://hal.archives-ouvertes.fr/hal-02323917
Publikováno v:
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⟩
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⟩
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 a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::457875c783d656ceef80ae6e476e11e5
https://hal.archives-ouvertes.fr/hal-02326725/file/2019_RodriguezDuarteTransforms.pdf
https://hal.archives-ouvertes.fr/hal-02326725/file/2019_RodriguezDuarteTransforms.pdf
Autor:
Matthias Delescluse, Nicolas Chamot-Rooke, Siegfried Lallemant, Philippe Huchon, Marc Fournier, Mathieu Rodriguez, Sébastien Zaragosi, Nicolas Mouchot
Publikováno v:
Tectonophysics
Tectonophysics, Elsevier, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
Tectonophysics, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
Tectonophysics, Elsevier, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
Tectonophysics, 2014, pp.1-49. ⟨10.1016/j.tecto.2014.08.001⟩
International audience; The Dalrymple Trough is a 150-km-long, 30-km-wide basin located at the northern termination of the Owen Fracture Zone (OFZ), which is the present-day active India-Arabia plate boundary. The Dalrymple Trough is closely associat
Publikováno v:
Tectonics. 32:1343-1357
[1] Pull-apart basins are common features observed at releasing bends along major strike-slip faults. The formation and structural evolution of such basins have mostly been investigated in the continental domain and by sandbox laboratory experiments
Autor:
Thomas François, Philippe Huchon, Matthias Delescluse, Marc Fournier, Mathieu Rodriguez, Nicolas Chamot-Rooke
Publikováno v:
Marine and Petroleum Geology
Marine and Petroleum Geology, Elsevier, 2016, 72, pp.336-358. ⟨10.1016/j.marpetgeo.2016.02.019⟩
Marine and Petroleum Geology, 2016, 72, pp.336-358. ⟨10.1016/j.marpetgeo.2016.02.019⟩
Marine and Petroleum Geology, Elsevier, 2016, 72, pp.336-358. ⟨10.1016/j.marpetgeo.2016.02.019⟩
Marine and Petroleum Geology, 2016, 72, pp.336-358. ⟨10.1016/j.marpetgeo.2016.02.019⟩
International audience; The location of the India-Arabia plate boundary prior to the formation of the Sheba ridge in the Gulf of Aden is a matter of debate. A seismic dataset crossing the Owen Fracture Zone, the Owen Basin, and the Oman Margin was ac
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bac870dc75e6570ebc66b650c5a7d74f
https://hal.archives-ouvertes.fr/hal-01396314
https://hal.archives-ouvertes.fr/hal-01396314
Autor:
Marc Fournier, Mathieu Rodriguez, Julien Bourget, Nicolas Chamot-Rooke, Matthias Delescluse, Philippe Huchon, Sébastien Zaragosi
Publikováno v:
Marine Geology
Marine Geology, Elsevier, 2016, 381, pp.1-16. ⟨10.1016/j.margeo.2016.08.004⟩
Marine Geology, 2016, 381, pp.1-16. ⟨10.1016/j.margeo.2016.08.004⟩
Marine Geology, Elsevier, 2016, 381, pp.1-16. ⟨10.1016/j.margeo.2016.08.004⟩
Marine Geology, 2016, 381, pp.1-16. ⟨10.1016/j.margeo.2016.08.004⟩
International audience; The relationships between oceanic circulation in the Arabian Sea and Late Cenozoic climate changes, including variations in monsoon intensity at the million year time-scale, remain poorly investigated. Using multibeam and seis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aac969843162a3705b05e59626192644
https://hal.archives-ouvertes.fr/hal-01396303
https://hal.archives-ouvertes.fr/hal-01396303