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The AAPG/Datapages Combined Publications Database

Journal of Petroleum Geology

Abstract

Journal of Petroleum Geology, Vol.18, No.4, pp. 439-452, 1995

©Copyright 2000 Scientific Press, Ltd.

ORIGIN OF THE MID-YPRESIAN JIRANI DOLOMITE--
A MAJOR RESERVOIR ROCK IN THE NW LIBYA OFFSHORE

I.Y. Mriheel* and J.M. Anketell**

* Petroleum Research Centre, PO Box 6431, Tripoli, Libya.

** Dept. of Geology, University of Manchester, Oxford Road, Manchester M13 9PL.


Abstract

The Jirani Dolomite was formed during a major relative fall in sea-level in middle Ypresian (early Eocene) times, in shallow, hypersaline lagoons on a restricted shallow platform, where supratidal and intertidal and semi-arid to arid conditions predominated localisation of the shallow lagoonal facies to the region of the Jifarah Trough suggests that restriction was caused by downwarp relative to mild uplift of the Jifarah Platform to the north.

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