Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Caroline Huguen"'
Publikováno v:
Solid Earth
Solid Earth, European Geosciences Union, 2021, 12 (5), pp.1211-1232. ⟨10.5194/se-12-1211-2021⟩
Solid Earth, Vol 12, Pp 1211-1232 (2021)
Solid Earth, 2021, 12 (5), pp.1211-1232. ⟨10.5194/se-12-1211-2021⟩
Solid Earth, European Geosciences Union, 2021, 12 (5), pp.1211-1232. ⟨10.5194/se-12-1211-2021⟩
Solid Earth, Vol 12, Pp 1211-1232 (2021)
Solid Earth, 2021, 12 (5), pp.1211-1232. ⟨10.5194/se-12-1211-2021⟩
Transform margins represent ∼ 30 % of non-convergent margins worldwide. Their formation and evolution have traditionally been addressed through kinematic models that do not account for the mechanical behaviour of the lithosphere. In this study, we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aebcbaa0ec2be9d31b58f7e8edcf7b19
https://hal.archives-ouvertes.fr/hal-03243028/document
https://hal.archives-ouvertes.fr/hal-03243028/document
Transform margins represent ~30 % of the non-convergent margins worldwide. Their formation and evolution have long been addressed through kinematic models that do not account for the mechanical behaviour of the lithosphere. In this study, we use high
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cb49ed0f3ff3f338e55102214dc72b0
https://doi.org/10.5194/se-2021-18
https://doi.org/10.5194/se-2021-18
Publikováno v:
Sedimentary Geology. 228:229-245
During the last 10 years several marine geological/geophysical surveys conducted on the Nile deep-sea fan have provided much new information about the large fluid seepage phenomenon, which characterizes this passive margin segment. Among the data, mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1fac606549d3e1426f114a9b4a7fc25d
https://doi.org/10.1016/j.sedgeo.2010.04.014
https://doi.org/10.1016/j.sedgeo.2010.04.014
Publikováno v:
Tectonics. 20:959-975
The Ivory Coast-Ghana margin is a typical transform margin along which large-scale tectonism has been well documented. The Cretaceous sediments of the Ivory Coast-Ghana transform margin were subjected to numerous tectonic, gravitational, and hydrothe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d7a8c5533cd51efb8c63f57114754a33
https://doi.org/10.1029/2001tc900015
https://doi.org/10.1029/2001tc900015
Autor:
Jean Mascle, Caroline Huguen
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 332:553-560
Between 23°30 and 25°30 Long East, i.e. over a distance of approximately 200 km, the morphology, sedimentary cover and geological structures of the continental margin of Libya have been analysed using swath bathymetry and seismic reflection data re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44176f931ea7ff46df7e4d21299fd3ea
https://doi.org/10.1016/s1251-8050(01)01575-0
https://doi.org/10.1016/s1251-8050(01)01575-0
Autor:
Jean Benkhelil, Caroline Huguen, Eric Chaumillon, J.M. Woodside, Achim J Kopf, Jean Mascle, A. Volkonskaia
Publikováno v:
Huguen, C, Mascle, J, Chaumillon, E, Woodside, J M, Benkhelil, J, Kopf, A & Volkonskaia, A 2001, ' Deformational styles of the eastern Mediterranean Ridge and surroundings from combined swath mapping and seiemic reflection profiling ', Tectonophysics, vol. 343, pp. 21-47 . https://doi.org/10.1016/S0040-1951(01)00185-8
Tectonophysics, 343, 21-47. Elsevier
Tectonophysics
Tectonophysics, Elsevier, 2001, 343 (1-2), pp.21-47. ⟨10.1016/S0040-1951(01)00185-8⟩
Tectonophysics, 343, 21-47. Elsevier
Tectonophysics
Tectonophysics, Elsevier, 2001, 343 (1-2), pp.21-47. ⟨10.1016/S0040-1951(01)00185-8⟩
Recent swath mapping and seismic reflection profiling across the eastern(Levantine) branch of the Mediterranean Ridge (MR), in the eastern Mediterranean Sea, illustrate a strong variability of the deformational styles that characterize this precollis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::527e4d846030fd6645dab9923a9b66f6
https://research.vu.nl/en/publications/f8fb87c5-8afa-4ea5-9359-9240acdfc508
https://research.vu.nl/en/publications/f8fb87c5-8afa-4ea5-9359-9240acdfc508
Publikováno v:
Marine Geology, 165, 1-12. Elsevier
Woodside, J M, Mascle, J, Huguen, C & Volkonskaia, A 2000, ' The Rhodes Basin, a Post-Miocene Tectonic Trough ', Marine Geology, vol. 165, pp. 1-12 . https://doi.org/10.1016/S0025-3227(99)00140-1
Woodside, J M, Mascle, J, Huguen, C & Volkonskaia, A 2000, ' The Rhodes Basin, a Post-Miocene Tectonic Trough ', Marine Geology, vol. 165, pp. 1-12 . https://doi.org/10.1016/S0025-3227(99)00140-1
New light is shed on the enigmatic Rhodes deep marine basin by a set of underway geophysical data across it, including swath bathymetry, seismic reflection profiles, gravity and magnetic data. This deep trough (as much as 4485 m) to the east of the I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::98d5f36ee4efe763767c585fec7e14cd
https://doi.org/10.1016/s0025-3227(99)00140-1
https://doi.org/10.1016/s0025-3227(99)00140-1
Autor:
S. Gontharet, Ingo Klaucke, Germain Bayon, Joel Etoubleau, Hélène Ondréas, K. Olu-Le Roy, Lies Loncke, Jean-Paul Foucher, Emmanuelle Ducassou, Sébastien Migeon, Jean Mascle, Stéphanie Dupré, Gideon M. Henderson, Caroline Huguen, Myriam Sibuet, Jean-Claude Caprais, J.M. Woodside, Sébastien Duperron, Yves Fouquet, Alina Stadnitskaia, Catherine Pierre
Publikováno v:
Marine Geology
Marine Geology, 2009, 261 (1), pp.92-104. ⟨10.1016/j.margeo.2008.10.008⟩
Marine Geology (0025-3227) (Elsevier), 2009-06, Vol. 261, N. 1-4, P. 92-104
Marine Geology, 261 (1-4). pp. 92-104.
Marine Geology, 261, 92-104. Elsevier
Marine Geology, Elsevier, 2009, 261 (1), pp.92-104. ⟨10.1016/j.margeo.2008.10.008⟩
Bayon, G, Loncke, L, Dupre, S, Caprais, J-C, Ducassou, E, Duperron, S, Etoubleau, J, Foucher, J-P, Fouquet, Y, Gontharet, S, Henderson, G M, Huguen, C, Klaucke, I, Mascle, J, Migeon, S, Olu-Le Roy, K, Ondreas, H, Pierre, C, Sibuet, M, Stadnitskaia, A & Woodside, J M 2009, ' Multi-disciplinary investigation of fluid seepage on an unstable margin: The case of the Centre Nile deep sea fan ', Marine Geology, vol. 261, pp. 92-104 . https://doi.org/10.1016/j.margeo.2008.10.008
Marine Geology, 2009, 261 (1), pp.92-104. ⟨10.1016/j.margeo.2008.10.008⟩
Marine Geology (0025-3227) (Elsevier), 2009-06, Vol. 261, N. 1-4, P. 92-104
Marine Geology, 261 (1-4). pp. 92-104.
Marine Geology, 261, 92-104. Elsevier
Marine Geology, Elsevier, 2009, 261 (1), pp.92-104. ⟨10.1016/j.margeo.2008.10.008⟩
Bayon, G, Loncke, L, Dupre, S, Caprais, J-C, Ducassou, E, Duperron, S, Etoubleau, J, Foucher, J-P, Fouquet, Y, Gontharet, S, Henderson, G M, Huguen, C, Klaucke, I, Mascle, J, Migeon, S, Olu-Le Roy, K, Ondreas, H, Pierre, C, Sibuet, M, Stadnitskaia, A & Woodside, J M 2009, ' Multi-disciplinary investigation of fluid seepage on an unstable margin: The case of the Centre Nile deep sea fan ', Marine Geology, vol. 261, pp. 92-104 . https://doi.org/10.1016/j.margeo.2008.10.008
We report on a multidisciplinary study of cold seeps explored in the Central Nile deep-sea fan of the Egyptian margin. Our approach combines in situ seafloor observation, geophysics, sedimentological data, measurement of bottom-water methane anomalie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c1dafc75cd4c3dafb15dad8618fb3a6b
http://ora.ox.ac.uk/objects/uuid:ecd56b7c-076b-4e6a-b6cd-ab4177f42ada
http://ora.ox.ac.uk/objects/uuid:ecd56b7c-076b-4e6a-b6cd-ab4177f42ada
Autor:
S. Gontharet, Jean-Paul Foucher, Hélène Ondréas, Antje Boetius, Ioanna Bouloubassi, Lies Loncke, J.M. Woodside, Caroline Huguen, M. Thouement, Stéphanie Dupré, Catherine Pierre, G. J. de Lange, Germain Bayon, Jean Mascle, Jean-Claude Caprais, Yves Fouquet, Alina Stadnitskaia
Publikováno v:
Marine Geology (0025-3227) (Elsevier Science Bv), 2009-06, Vol. 261, N. 1-4, P. 138-152
Marine Geology
Marine Geology, 2009, 261 (1-4), pp.138-152. ⟨10.1016/j.margeo.2009.02.005⟩
Marine Geology, Elsevier, 2009, 261 (1-4), pp.138-152. ⟨10.1016/j.margeo.2009.02.005⟩
Huguen, C, Foucher, J-P, Mascle, J, Ondreas, H, Thouement, M, Gontharet, S, Stadnitskaia, A, Pierre, C, Bayon, G, Loncke, L, Boetius, A, Bouloubassi, I, de Lange, G, Caprais, J-C, Fouquet, Y, Woodside, J M & Dupre, S 2009, ' Menes caldera, a highly active site of brine seepage in the Eastern Mediterranean Sea: "In situ" observations from the NAUTINIL expedition (2003) ', Marine Geology, vol. 261, pp. 138-152 . https://doi.org/10.1016/j.margeo.2009.02.005
Marine Geology, 261, 138-152. Elsevier
Marine Geology
Marine Geology, 2009, 261 (1-4), pp.138-152. ⟨10.1016/j.margeo.2009.02.005⟩
Marine Geology, Elsevier, 2009, 261 (1-4), pp.138-152. ⟨10.1016/j.margeo.2009.02.005⟩
Huguen, C, Foucher, J-P, Mascle, J, Ondreas, H, Thouement, M, Gontharet, S, Stadnitskaia, A, Pierre, C, Bayon, G, Loncke, L, Boetius, A, Bouloubassi, I, de Lange, G, Caprais, J-C, Fouquet, Y, Woodside, J M & Dupre, S 2009, ' Menes caldera, a highly active site of brine seepage in the Eastern Mediterranean Sea: "In situ" observations from the NAUTINIL expedition (2003) ', Marine Geology, vol. 261, pp. 138-152 . https://doi.org/10.1016/j.margeo.2009.02.005
Marine Geology, 261, 138-152. Elsevier
Marine Geology, v. 261, n. 1-4, p. 138-152, 2009. http://dx.doi.org/10.1016/j.margeo.2009.02.005; International audience; This paper reports the first "in situ" seafloor observations of fluid escape structures in a fault-controlled caldera-type depre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e328bc5fc88a6d0c4f658944fc7cd762
https://archimer.ifremer.fr/doc/00000/11089/
https://archimer.ifremer.fr/doc/00000/11089/