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1-6 OF 6
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R. Schlich
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Journal Article
Application d'un modele numerique de calcul du champ de temperature dans les regions de Bains-les-Bains et Plombieres-les-Bains
Publisher: Société Géologique de France
Published: 01 November 1987
Bulletin de la Société Géologique de France (1987) III (6): 1041–1048.
Journal Article
Les campagnes du N. O. Jean Charcot sur le point triple de Rodriguez (Ocean Indien); premiers resultats
Publisher: Société Géologique de France
Published: 01 July 1987
Bulletin de la Société Géologique de France (1987) III (4): 693–697.
Journal Article
Les mouvements relatifs de l'Inde, de l'Afrique et de l'Eurasie
P. Patriat, J. Segoufin, R. Schlich, J. Goslin, Jean-Marie Auzende, P. Beuzart, J. Bonnin, J. L. Olivet
Publisher: Société Géologique de France
Published: 01 January 1982
Bulletin de la Société Géologique de France (1982) S7-XXIV (2): 363–373.
Journal Article
Mise en place et evolution des plateaux sous-marins de Madagascar et de Crozet
Publisher: Société Géologique de France
Published: 01 January 1981
Bulletin de la Société Géologique de France (1981) S7-XXIII (6): 609–618.
Journal Article
Le Maestrichtien du site 239 (D.S.D.P. ocean Indien) dans son cadre regional et son incidence sur l'echelle chronologique des inversions du champ magnetique terrestre
Publisher: Société Géologique de France
Published: 01 January 1979
Bulletin de la Société Géologique de France (1979) S7-XXI (1): 57–63.
Book Chapter
Microcontinental Margins
Series: AAPG Continuing Education Course Notes Series
Publisher: American Association of Petroleum Geologists
Published: 01 January 1977
DOI: 10.1306/CE5387C16
EISBN: 9781629812021
Abstract Elevated aseismic structures more or less isolated in the oceans have been often interpreted as microcontinents. They are particularly numerous in the Indian Ocean: Crozet Plateau, Kerguelen Plateau, Madagascar Plateau, Seychelles Plateau. Geophysical data show that some of these plateaus are true microcontinents (continental crust) while others are probably only elevated oceanic structures. Other examples are shown in the North Atlantic: The Jan Mayen Ridge in the Norwegian Sea and the Rockall Plateau. Sedimentation on the margins of true microcontinents are often characterized by well defined syn-rift deposits and pelagic post-opening sediments with few elastics due to the isolation from important land-masses.