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Abstract

Anhydrite is one of the most common porosity destroying minerals in ancient, arid climate carbonate reservoirs like the Arab and Khuff formations. Reservoir quality is inversely proportional to the amount of pore-filling and replacement anhydrite-after-gypsum.

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/content/papers/10.3997/2214-4609-pdb.287.1186119
2012-03-04
2026-01-17
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