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Abstract

The Late Jurassic Arab Formation is being developed in a major gas accumulation located onshore southern UAE. The reservoir intervals form a large scale shallowing-upward cycle capped by the widespread Hith anhydrite topseal. The lower Arab Formation consists of wackestones to mudstones of mid ramp to basinal setting (Arab D Member) overlain by foreshoal and oolitic grainstone shoal deposit of the Arab C Member. The succeeding Upper Arab (A & B Members) comprises alternations of dolomitic limestone and anhydrite of restricted lagoon to backshoal and sabkha / salina origin.

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/content/papers/10.3997/2214-4609.20142807
2012-12-09
2020-10-31
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20142807
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