Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Laurent Camera"'
Publikováno v:
Marine and Petroleum Geology. 23:297-315
Structural analysis of the Nile deep-sea fan (NDSF) indicates that post-Miocene deformation is largely controlled by down-slope movement above a Messinian salt layer. In contrast to other similar systems, the NDSF shows significant lateral asymmetry,
Autor:
Laurent Camera, Silvia Ceramicola, Jean Mascle, Daniel Praeg, Flore Mary, Stéphanie Dupré, Laetitia Brosolo
Publikováno v:
Geo-Marine Letters
Geo-Marine Letters, Springer Verlag, 2014, 34 (2-3), pp.89-110. ⟨10.1007/s00367-014-0356-4⟩
Geo-Marine Letters, 2014, 34 (2-3), pp.89-110. ⟨10.1007/s00367-014-0356-4⟩
Geo-marine Letters (0276-0460) (Springer), 2014-06, Vol. 34, N. 2-3, P. 89-110
Geo-Marine Letters, Springer Verlag, 2014, 34 (2-3), pp.89-110. ⟨10.1007/s00367-014-0356-4⟩
Geo-Marine Letters, 2014, 34 (2-3), pp.89-110. ⟨10.1007/s00367-014-0356-4⟩
Geo-marine Letters (0276-0460) (Springer), 2014-06, Vol. 34, N. 2-3, P. 89-110
International audience; Existing knowledge on the distribution of mud volcanoes (MVs) and other significant fluid/free gas-venting features (mud cones, mud pies, mud-brine pools, mud carbonate cones, gas chimneys and, in some cases, pockmark fields)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6fb4dd941651b6bf4357ba0637c1677f
https://hal.archives-ouvertes.fr/hal-01859771
https://hal.archives-ouvertes.fr/hal-01859771
Autor:
Lies Loncke, Olivier Sardou, Laurent Camera, Sébastien Migeon, Virginie Gaullier, Jean Mascle
Publikováno v:
Marine Geophysical Research
Marine Geophysical Research, Springer Verlag, 2006, 27 (1), pp.49-59. ⟨10.1007/s11001-005-1559-x⟩
Marine Geophysical Research, 2006, 27 (1), pp.49-59. ⟨10.1007/s11001-005-1559-x⟩
Marine Geophysical Research, Springer Verlag, 2006, 27 (1), pp.49-59. ⟨10.1007/s11001-005-1559-x⟩
Marine Geophysical Research, 2006, 27 (1), pp.49-59. ⟨10.1007/s11001-005-1559-x⟩
International audience; In the Eastern Mediterranean, offshore Egypt, the Nile continental margin is characterized by a large deep water turbiditic system known as the Nile Deep Sea Fan. This post-Miocene terrigenous construction covers an approximat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7bbabd563d4e2f10e9aeac0e306a957a
https://hal.archives-ouvertes.fr/hal-00407700
https://hal.archives-ouvertes.fr/hal-00407700