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The AAPG/Datapages Combined Publications Database

Journal of Petroleum Geology

Abstract

Journal of Petroleum Geology, Vol.14, No.1, pp. 93-102, 1991

©Copyright 2000 Scientific Press, Ltd.

TECTONIC SUBSIDENCE OF THE SIRTE BASIN, LIBYA

Y. D. Gumati* + and A. E. M. Nairn*

*Earth Sciences and Resources Institute, University of South Carolina, Columbia, SC 29208. USA.
+ Present address: Geology Department, UAE University, PO Box 1555, Al Ain, UAE.


Abstract

The Sirte Basin of Libya has a history of faulting and differential subsidence brought about by lithospheric extension during a 25 MM (million) year period beginning in the Late Cretaceous. The first phase of extension and initial subsidence, with faulting and graben formation, occurred from Cenomanian to Campanian times. Following extension, there occurred widespread thermally-driven subsidence from Maastrichtian through Eocene and Oligocene times, accounting for about Previous HithalfTop of the total subsidence.

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