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Sichler, Bertrand / Mascle, Jean / Cressard, Alain - 1972La comparaison d'un profil de sismique réflexion oblique avec les résultats d'Une station de sismique réfraction effectuée antérieurement permet de préciser l'extension probable de la faille « JeanCharcOt » vers le Nord-Est du fossé de Rockall.Contributeur (s):
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Olivet, Jean-louis / Auzende, Jean-marie / Mascle, Jean / Monti, S. / Pastouret, Léo / Pautot, Guy - 1971Recent data on the western Mediterranean basin (Joides cruise, Montadert et al., 1970, Auzende et al., 1971, Le Borgne et al., 1971) and its connection with the evolution of the Atlantic area (Le Pichon et al., 1970, Talwani et al., 1971, Le Pichon et al. in writing) lead us, like other authors (...Contributeur (s):
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Briseid, E. / Mascle, Jean - 1975Reconstructions of the continents prior to the opening of the Norwegian sea indicate an overlap between the Greenland and the Norwegian continental margins just west of the Barentz sea and imply that the basement of this area is of oceanic origin. Seismic profiling shows an oceanic-type basement...Contributeur (s):
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Mascle, Jean / Auroux, C - 1989During the Equamarge II cruise (February 4 to March 21, 1988), on board the R. V. "Jean Charcot", 12.500 kms of continuous geophysical profiling have been recorded along three sectors of the Equatorial Atlantic. Two segments of the West African transform margin have been intensively...Contributeur (s):
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Le Pichon, Xavier / Cressard, Alain / Mascle, Jean / Pautot, Guy / Sichler, Bertrand - 1970In 1921 the "Pourquoi pas?" undertook, under the authority of J. Charcot, an identification of the Rockall bank (2). The petrographic nature of this relief was studied by Lacroix (2) who concluded to aegirine granite dated, since then, by Miller (3) and Sabine (4), from the early Tertiary...Contributeur (s):
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Mascle, Jean - 1975Marine geophysical profiles off Niger Delta reveal the presence of diapiric structures beneath the continental margin. The hypothesis of a possible evaporitic layer is presented and discussed ; the general structure of the area is briefly compared to the structure of the northern margin of the gulf...Contributeur (s):
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Huguen, Caroline / Benkhelil, J / Giresse, P / Mascle, Jean / Muller, C / Woodside, John / Zitter, T / Charlou, Jean-luc - 2001In the eastern Mediterranean, numerous argilo-kinetic manifestations, commonly named 'mud volcanoes', have been identified and studied in some detail during the last twenty years using several techniques. The Medinaut survey (December 1998) has provided new insights into this phenomenon...Contributeur (s):
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Mascle, Jean - 1971In a previous article published in the "cahiers Océanographiques" XXII, 1 (January 1970), pp. 25-32, I described the broad lines of subactual sedimentation in and around the canyon of Toulon. This data had been collected during a drilling cruise conducted in October 1967. Out of the 41...Contributeur (s):
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Mascle, Jean / Smit, Albert F.j. - 1974Ferruginous sandstones and slightly metamorphosed sandstones have been dredged on the continental slope off the Ghanaian coast at depths of 3 500 to 2 000 m. Their attribution to the Paleozoic series known on dry land is not quite obvious, though some lithologic affinities exist. As a consequence,...Contributeur (s):
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Malod, J. / Mascle, Jean - 1975The main structural features of the continental margin off West Spitzberg are outlined. Seaward the Atka ridge has acted like a dam for the eastward-flowing sediments and thus helped to build up a large sedimentary basin, narrowing towards the North. Magnetic and seismic data show that the Atka...Contributeur (s):
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Sichler, Bertrand / Mascle, Jean / Cressard, Alain - 1972La comparaison d'un profil de sismique réflexion oblique avec les résultats d'Une station de sismique réfraction effectuée antérieurement permet de préciser l'extension probable de la faille « JeanCharcOt » vers le Nord-Est du fossé de Rockall.Contributeur (s):
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Gennesseaux, Maurice / Mascle, Jean - 2012International audienceContributeur (s):
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Werne, Josef P. / Haese, Ralf R. / Zitter, Tiphaine / Aloisi, Giovanni / Bouloubassi, Ionna / Heijs, Sander / Fiala-Médioni, Aline / Pancost, Richard D. / Sinninghe Damsté, Jaap S. / De Lange, Gert / Forney, Larry J. / Gottschal, Jan C. / Foucher, Jean-Paul / Mascle, Jean / Woodside, John - 2015International audienceContributeur (s):
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Dano, Alexandre / Praeg, Daniel / Migeon, Sebastien / Augustin, Jean-marie / Ceramicola, Silvia / Ketzer, Joao Marcelo / Augustin, Adolfo Herbert / Ducassou, Emmanuelle / Mascle, Jean - 2015The central Nile Deep-Sea Fan contains a broad area of seabed destabilisation in association with fluid seepage: slope-parallel sediment undulations are associated with multibeam high-backscatter patches (HBPs) related to authigenic carbonates. During the 2011 APINIL campaign, a deep-towed sidescan...Contributeur (s):
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Pierre, Catherine / Bayon, Germain / Blanc-valleron, Marie-madeleine / Mascle, Jean / Dupre, Stephanie - 2014On the passive margin of the Nile deep-sea fan, the active Cheops mud volcano (MV; ca. 1,500 m diameter, ~20–30 m above seafloor, 3,010–3,020 m water depth) comprises a crater lake with hot (up to ca. 42 °C) methane-rich muddy brines in places overflowing down the MV flanks. During the Medeco2...Contributeur (s):