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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The paper gives a description of the reservoir rocks of three fields, Masjid-i-Sulaiman, Haft Kel, and Naft Khaneh. The reservoir rock is a limestone of Lower Miocene age called the Asmari limestone. It is a fine-grained foraminiferal limestone, mostly of low porosity, and the porosity of the rock is independent of the degree of dolomitization. Fracturing of the rock is the most important factor governing production.
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