Download PDF by Carman P.C.: Flow of gases through porous media

By Carman P.C.

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This recognition is made difficult by the tendency for such events to coincide with, or to be close to, zones of present activity, as, for example, the late Paleozoic to Cenozoic history of the Zagros Crush Zone with the opening and subsequent closure of the Neotethys. The Arabian Peninsula forms the nuclear region for the Middle East. It is generally separated into the exposed Precambrian part or shield, and the sediment-covered platform. The Precambrian basement generally dips gently to the north-northeast and east, as the sediment cover thickens progressively from less than 1,500 m (4,920 ft) to more than 10,940 m (35,883 ft) in the vicinity of the Arabian Gulf (Fig.

700 Z u b a i r F o r m a t i o n . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 700 S h u a i b a F o r m a t i o n . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 7 00 N a h r I m r F o r m a t i o n . . . .

S. X x x : eD: . L X X X X . . . ~ Precambrian rocks with Mesozoic-Cenozoic cover of stable shelf [' RO [ RndiolarianophioUte complex (mainly Upper Cretaceous) '/"-/" Oceanic crust within the Gulf of Aden ~and Red Sea Faults Thrust fault Rift fault ~Xx x x~] Precambrianrocks x/ Fig. 3. Structural elements of the Middle East (modified from Henson, 1951; and Beydoun, 1988). source regions from trade routes. But, as the supplies from the more traditional sources begin to diminish, the potential of the region can be expected to attract more attention.

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Flow of gases through porous media by Carman P.C.


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