Tectonic activity in West Africa and the Gulf of Guinea since Jurassic times - An explanation based on membrane tectonics

Details Tectonic activity in West Africa and the Gulf of Guinea since Jurassic times - An explanation based on membrane tectonics Tectonic activity in West Africa and the Gulf of Guinea since Jurassic times - An explanation based on membrane tectonics

Feb 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978e%26psl..38..298f&link_type=abstract

Earth and Planetary Science Letters, Volume 38, Issue 2, p. 298-300.

Computer Science

Scientific paper

Membrane stresses generated by the northward movement of the African plate over a non-spherical earth provide a possible explanation for tectonic activity in West Africa and the Gulf of Guinea. The change from a compressional regime (90 m.y. to 40 m.y.) to an extensional regime (40 m.y. to present day) occurred when the effective mechanical centre of the African plate crossed the equator.

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