作者: J.-C. Maurin , R. Guiraud
DOI: 10.1016/0899-5362(90)90064-L
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摘要: Abstract New structural investigations performed within the Barremo-Aptian basins of Northern Cameroon allow us to specify their tectono-sedimentary history. They are asymmetrical synsedimentary synclines superimposed on half-grabens. The lattr represent sinistral transtensive structures which opened in response a N160 extension that occurred during times. This opening regime is different from large Albo-Aptian trough such as Benue trough. According our recent hypothesis these successie extensions could be related diachronic evolution South Atlantic Ocean.