FN Archimer Export Format PT J TI Facies evolution and carbonate dissolution cycles in sediments from basins and continental margins of the eastern south atlantic since early cretaceous BT AF 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. AS 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:; FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:; TC 0 UR https://archimer.ifremer.fr/doc/1975/publication-5090.pdf LA English DT Article DE ;Histoire Ifremer AB 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] PY 1975 SO IX CONGRES INTERNATIONAL DE SEDIMENTOLOGIE ID 5090 ER EF