Sedimentological, petrographic and geochemical constraints on the origin of extensive dolomites of the Cretaceous Sidi as Sid Formation (Ain Tobi Member) in NW Libya
The Cretaceous Sidi as Sid Formation outcrops in the Jabal Nafusah Escarpment, northwest Libya. It is composed of two members; the lower Ain Tobi Member and the upper Yifran Member. The Yifran Member consists of marl, dolomitic limestone and gypsum. The Ain Tobi Member is composed entirely of dolomi...
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University of Leicester
1996
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.554266 |