Titlebook: Geology of the Northwest African Continental Margin; Ulrich Rad,Karl Hinz,Eugen Seibold Conference proceedings 1982 Springer-Verlag Berlin

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Mesozoic-Cenozoic Development of the Eastern North American and Northwest African Continental Marginaouira (or Atlas) Basin of Central Morocco (“northern transect”) in the east; the Georges Bank Basin on the northeastern U.S. shelf with the Tarfaya-Aaiun Basin of Southern Morocco (“central transect”) and, finally, the Blake Plateau Basin of the southeastern U.S. shelf with the Mauritania-Senegal B

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Wallow

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978-3-642-68411-1Springer-Verlag Berlin Heidelberg 1982

Cocker

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https://doi.org/10.1007/978-3-540-92725-9egment in the south, northward to the Tafelney Plateau, the Essaouira segment, the Mazagan Plateau, and the Pre-Rif segment..The dominating structural unit of the Moroccan continental margin is a NNE-trending zone of salt diapirs. This zone starts southeast of Fuerteventura and continues to the nort

Charlatan

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