Facies evolution and carbonate dissolution cycles in sediments from basins and continental margins of the eastern south atlantic since early cretaceous
Type | Article | ||||||||
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Date | 1975 | ||||||||
Language | English | ||||||||
Author(s) | Melguen Marthe, Bolli Hans M., Ryan William B.F., Foresman James B., Hottman William E., Kagami Hideo, Longoria José F., Mc Knight Brian K., Natland James, Proto Decpia Franca, Siesser William G. | ||||||||
Source | IX CONGRES INTERNATIONAL DE SEDIMENTOLOGIE, 1975 | ||||||||
Mot-Clé(s) | Histoire Ifremer | ||||||||
Abstract | The evolution of the sedimentary facies in the southeast Atlantic Ocean since the Cretaceous is strongly correlated to the structural history of this ocean. Since the first observations of Wegener (1929) about the continental drift, numerous authors (Bullard et al., 1965 ; Almeida and Black, 1967 ; Hurley et al., 1967 ; Hurley, 1968 ; Reyment and Tait, 1972 ; Krommelbein and Wenger, 1966 ; Maack, 1969) have confirmed the hypothesis of the separation of both continents, Africa and South America. [NOT CONTROLLED OCR] | ||||||||
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