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Registros recuperados: 28
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Les marges continentales transformantes ouest - africaines : Guinée, Côte d'Ivoire, Ghana et la zone de la fracture de la Romanche. Campagne Equamarge II : rapport scientifique ArchiMer
Mascle, Jean; Auroux, C.
During 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 surveyed off Guinea and off Ivory Coast and Ghana. The active Romanche fracture zone has been surveyed in details on a distance of about 100 kms. These data (multibeam bathymetry, continuous seismic profiling, magnetism and gravity) have been supplemented by 16 geological stations (dredging and coring). This report gives a synthetic review of the onboard analysis and allows to better understand the geological structures of the three surveyed areas. [NOT CONTROLLED OCR]
Tipo: Text Palavras-chave: Atlantique équatorial; Ouest Afrique; Bathymétrie sismique réflexion; Zone de fracture océanique; Marges continentales transformantes.
Ano: 1989 URL: http://archimer.ifremer.fr/doc/1989/rapport-4461.pdf
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Échantillons rocheux provenant de « volcans de boue » de Méditerranée orientale ArchiMer
Huguen, Caroline; Benkhelil, J; Giresse, P; Mascle, Jean; Muller, C; Woodside, John; Zitter, T; The Medinaut Scientific Party,.
In 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 through twenty deep dives performed with the submersible Nautile within two areas particularly active in terms of mud expulsions: the central Mediterranean ridge south of Crete, and the Anaximander mountains area, south of Turkey. The morphology, petrography, microstructure and biostratigraphy of different clasts sampled in the two areas helped to better understand the mud volcano formation and subsequent evolution. Paleoenvironmental conditions, ranging from deep marine...
Tipo: Text Palavras-chave: Clasts; Eastern Mediterranean; Deep dives; 'mud volcanoes'.
Ano: 2001 URL: http://archimer.ifremer.fr/doc/00068/17931/15469.pdf
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Diapiric structures off niger delta ArchiMer
Mascle, Jean; Bornhold, Brian D.; Renard, Vincent.
Several marine geophysical profiles off the southern part of the Niger delta reveal the presence of diapiric structures beneath the continental slope and rise. The origin of the diapiric material appears to be deep in the sedimentary section and is believed to be of Aptian-Albian age. If this hypothesis is correct, the presence of evaporite basins, known between angola and Gabon, can be extended as far north as the Niger delta. [NOT CONTROLLED OCR]
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1973 URL: http://archimer.ifremer.fr/doc/1973/publication-5119.pdf
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Nature de la pente continentale au Sud du Cap des Trois Pointes (Ghana, Afrique) ArchiMer
Mascle, Jean; Smit, Albert F.j..
Ferruginous 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, the continental slope in this area, which corresponds to the structural continuation of the Romanche fracture zone, is partially of sedimentary nature.
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1974 URL: http://archimer.ifremer.fr/doc/1974/publication-5442.pdf
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MEDECO Leg 2 cruise report. R/V Pourquoi pas ? 02 to 30 November 2007 Rhodes-Toulon ArchiMer
Pierre, Catherine; Mascle, Jean; Dupre, Stephanie.
The MEDECO Leg 2 cruise followed the MEDECO Leg 1 cruise that had crossed the Mediterranean Sea from the west to the east to study benthic communities of the Var canyon, deep corals found on the Calabrian Margin and cold seep ecosystems of the Mediterranean Ridge. The main objective of the MEDECO Leg 2 cruise was to study and compare, using a multidisciplinary approach, the structure and dynamics of deep-sea ecosystems at various active cold seep sites from the Nile deep sea fan and the Calabrian Arc, in the Eastern Mediterranean sea. During MEDECO Legs 1 & 2, a multiscale strategy was promoted to integrate (1) a high resolution cartography of geological structures (km2 scale), (2) a detailed mapping, including video imagery, of smaller-scale areas...
Tipo: Text
Ano: 2008 URL: http://archimer.ifremer.fr/doc/00134/24550/22583.pdf
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Sismique réflexion oblique dans le fossé de Rockall ArchiMer
Sichler, Bertrand; Mascle, Jean; Cressard, Alain.
La 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.
Tipo: Text
Ano: 1972 URL: http://archimer.ifremer.fr/doc/00318/42966/42472.pdf
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Les structures diapiriques du delta du Niger ArchiMer
Mascle, Jean.
Marine 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 of Mexico where well-known evaporitic structures occur along the whole margin. [NOT CONTROLLED OCR]
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1975 URL: http://archimer.ifremer.fr/doc/1975/publication-4984.pdf
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Structure de la marge continentale norvégienne au débouché de la mer de Barentz ArchiMer
Briseid, E.; Mascle, Jean.
Reconstructions 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 covered by thick Tertiary sediments. The sedimentary supply is related to the geological history of the Barentz sea where only little unconsolidated sediments are known. Further south the structures of the present margin are directly related to the early opening of the Norwegian sea. [NOT CONTROLLED OCR]
Tipo: Text Palavras-chave: Histoire Ifremer.
Ano: 1975 URL: http://archimer.ifremer.fr/doc/1975/publication-5440.pdf
Registros recuperados: 28
Primeira ... 12 ... Última
 

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