Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Marie-Eva Epin"'
Publikováno v:
Marine and Petroleum Geology
Marine and Petroleum Geology, Elsevier, 2021, 128, pp.105005. ⟨10.1016/j.marpetgeo.2021.105005⟩
Marine and Petroleum Geology, Elsevier, 2021, 128, pp.105005. ⟨10.1016/j.marpetgeo.2021.105005⟩
In this study, we present an interpretation of a 3D depth-migrated dataset imaging the Ocean Continent-Transition (OCT) of the southern Gabon margin. Located in an area where salt is not strongly overflowing the OCT, it allows the geometrical relatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ad6ad71b206d7edcc8294da5259f0640
https://hal.archives-ouvertes.fr/hal-03514410
https://hal.archives-ouvertes.fr/hal-03514410
Publikováno v:
Journal of the Geological Society. 177:667-669
Dr. Giancarlo Molli constructively replied to our paper ‘Breakup continents at magma poor rifted margins: a seismic v. outcrop perspective’ (Molli 2020) with a twofold argument (i) criticizing the collection of data, and, more importantly, (ii) q
Autor:
Marc Ulrich, Méderic Amann, Gianreto Manatschal, Daniel Sauter, Marie-Eva Epin, Eric Pelt, Julia Autin
Publikováno v:
Terra Nova
Terra Nova, Wiley-Blackwell, 2019, 32 (1), pp.75-88. ⟨10.1111/ter.12438⟩
Terra Nova, Wiley-Blackwell, 2019, 32 (1), pp.75-88. ⟨10.1111/ter.12438⟩
International audience; Basalts exposed in the Platta and Tasna nappes (SE Switzerland) derive from the Alpine-Tethys Ocean-Continent Transitions (OCT) and overlie SubContinental Lithospheric Mantle (SCLM). We show that the trace element signatures o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f970dfd9ed8ede36e3c5bbca5215054f
https://hal-insu.archives-ouvertes.fr/insu-02456734/document
https://hal-insu.archives-ouvertes.fr/insu-02456734/document
Autor:
M. Lescanne, Marie-Eva Epin, Charlotte Ribes, Antoine Clausse, Gianreto Manatschal, T. Guffon, M. Amman
Publikováno v:
International Journal of Earth Sciences
International Journal of Earth Sciences, Springer Verlag, 2019, 108 (8), pp.2443-2467. ⟨10.1007/s00531-019-01772-0⟩
International Journal of Earth Sciences, Springer Verlag, 2019, 108 (8), pp.2443-2467. ⟨10.1007/s00531-019-01772-0⟩
Despite the fact that many studies have investigated mantle exhumation at ultra-slow-spreading ridges and magma-poor rifted margins, there are still numerous questions concerning the 3D architecture, magmatic, fluid, and thermal evolution of these do
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ada39660f7c7a02930659c0ebc827b9e
https://hal.archives-ouvertes.fr/hal-03102454
https://hal.archives-ouvertes.fr/hal-03102454
Autor:
Jean-François Ghienne, Charlotte Ribes, Nicolò Incerpi, Garry D. Karner, Marie-Eva Epin, Patricio H. Figueredo, Gianreto Manatschal, Christopher A. Johnson
Publikováno v:
International Journal of Earth Sciences
International Journal of Earth Sciences, Springer Verlag, 2019, 108 (6), pp.2071-2095. ⟨10.1007/s00531-019-01750-6⟩
International Journal of Earth Sciences, Springer Verlag, 2019, 108 (6), pp.2071-2095. ⟨10.1007/s00531-019-01750-6⟩
International audience; To understand the overall spatial and temporal evolution and resulting sedimentary stacking patterns within an evolving hyper-extended rift system, we investigated the Austroalpine and Upper Penninic nappes in the Central Alps
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::962abdf607401ab32cd6b110554a4649
https://hal.archives-ouvertes.fr/hal-02412943
https://hal.archives-ouvertes.fr/hal-02412943
Autor:
Gianreto Manatschal, Marie-Eva Epin
Publikováno v:
Tectonics
Tectonics, American Geophysical Union (AGU), 2018, ⟨10.1029/2018TC005125⟩
Tectonics, American Geophysical Union (AGU), 2018, ⟨10.1029/2018TC005125⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cff839e15949038d5f4fe4a8172db243
https://hal.archives-ouvertes.fr/hal-03102512/file/2018TC005125.pdf
https://hal.archives-ouvertes.fr/hal-03102512/file/2018TC005125.pdf
Publikováno v:
Journal of the Geological Society
Journal of the Geological Society, Geological Society of London, 2018, 175 (6), pp.875-882. ⟨10.1144/jgs2018-041⟩
Journal of the Geological Society, Geological Society of London, 2018, 175 (6), pp.875-882. ⟨10.1144/jgs2018-041⟩
The breakup of continents at magma-poor rifted margins is a complex, yet little understood process accounting for intricate interactions between tectonic and magmatic processes. Whereas high resolution seismic data may resolve the first order archite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::38281f5aa0c5f4d9f49c8ff80abeed48
https://hal.archives-ouvertes.fr/hal-03102524
https://hal.archives-ouvertes.fr/hal-03102524
Autor:
Rémi Coltat, Philippe Boulvais, yannick branquet, Joseph Collot, Marie-Eva Epin, Gianreto Manatschal
Publikováno v:
26ème Réunion des Sciences de la terre-RST
26ème Réunion des Sciences de la terre-RST, Oct 2018, Lille, France. pp.220
HAL
26ème Réunion des Sciences de la terre-RST, Oct 2018, Lille, France. pp.220
HAL
International audience; Les transitions océan-continent (OCT) sont reconnues comme des environnements propices à la formation et au piégeage d’hydrocarbures. Ainsi lors des dernières décennies, de nombreuses études ont été entreprises à tr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bd887d65299fa445a3e87f88f86e8d7a
https://hal-insu.archives-ouvertes.fr/insu-01916036
https://hal-insu.archives-ouvertes.fr/insu-01916036
Autor:
Morgane Gillard, Nick Kusznir, Michael Nirrengarten, Julia Autin, Marie-Eva Epin, Gianreto Manatschal, Julie Tugend, Caroline Harkin, Ken McDermott, Daniel Sauter
Publikováno v:
The Geological Society, London, Special Publications
The Geological Society, London, Special Publications, Geological Society of London, 2018, pp.SP476.9. ⟨10.1144/SP476.9⟩
The Geological Society, London, Special Publications, Geological Society of London, 2018, 476, pp.23-47. ⟨10.1144/SP476.9⟩
Geological Society, London, Special Publications
The Geological Society, London, Special Publications, Geological Society of London, 2018, pp.SP476.9. ⟨10.1144/SP476.9⟩
The Geological Society, London, Special Publications, Geological Society of London, 2018, 476, pp.23-47. ⟨10.1144/SP476.9⟩
Geological Society, London, Special Publications
Rifted margins are commonly defined as magma-poor or magma-rich archetypes based on their morphology. We re-examine the prevailing model inferred from this classification that magma-rich margins have excess decompression melting at lithospheric break
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::648458d9e7ec3612dfd3e0f5d6ed95a0
https://hal.archives-ouvertes.fr/hal-02371095
https://hal.archives-ouvertes.fr/hal-02371095
Autor:
Morgane Gillard, Daniel Sauter, Julie Tugend, Simon Tomasi, Marie-Eva Epin, Gianreto Manatschal
Publikováno v:
Scientific Reports
Scientific Reports, Nature Publishing Group, 2017, 7 (1), ⟨10.1038/s41598-017-15522-2⟩
Scientific Reports, Vol 7, Iss 1, Pp 1-6 (2017)
Scientific Reports, Nature Publishing Group, 2017, 7 (1), ⟨10.1038/s41598-017-15522-2⟩
Scientific Reports, Vol 7, Iss 1, Pp 1-6 (2017)
International audience; Oceanic crust is continuously created at mid-oceanic ridges and seafloor spreading represents one of the main processes of plate tectonics. However, if oceanic crust architecture, composition and formation at present-day ocean