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

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Common Picture Communication Systems,up to 4 km of Early Cretaceous Wealden-type deltaic sediments. Rollover structures between antithetic growth faults produced the “lower slope anticline” and a convex Cretaceous paleoslope. We recognized no salt diapirs, but local piercement structures probably caused by mobilized Early Cretaceous pr

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https://doi.org/10.1007/978-3-319-48042-8 The sections are based mainly on joint refraction surveys of the Institut fur Geophysik (Hamburg) and the Federal Institute for Geosciences and Natural Resources (BGR, Hannover) and additional information from published refraction work in the survey areas..On both sections rift basins were crossed,

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Multiband Microscanning Sensor,ean off West Africa as reflected by the calcareous nannoplankton and the planktonic foraminifera. The zonations adopted from various sources are partly emended. The Cretaceous epoch is divided into 21 nanno-zones and/or 30 foram-zones, however, not all zones could be distinguished in the study area.

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https://doi.org/10.1007/978-3-322-84821-51977). Johnson (1976) suggested that the poor preservation of siliceous skeletons may be due to the relatively small amount of silica being deposited in the Atlantic Basin. Examinations of the Mesozoic DSDP cores from the Northwest African continental margin again confirm this observation. With few

外向者

https://doi.org/10.1007/978-1-4899-2031-7The Northwest African continental margin has many features which parallel those of the Northeast American continental margin, both in structure and evolution. However, up to the present time, many aspects of orogenic and volcanic activity and of climatic and oceanographic evolution have differed.

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Atlas and Atlantic — Structural RelationsIntracratonic mountain building processes and ocean genesis may occasionally have the same origin. Our results on the evolution of the High Atlas imply that vertical movements should not be neglected in future discussions on global tectonics.