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Abstract

The Lower part of Middle Minagish Oolite reservoir, MO-Layer 13 consists largely of fine-grained, tight bioturbated, lime packstones. Deposition of this interval took place on a shallow very gently sloping outer-ramp; these intervals are more susceptible to stylolitization and/or dolomitization.

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/content/papers/10.3997/2214-4609-pdb.287.1216962
2012-03-04
2025-06-16
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/content/papers/10.3997/2214-4609-pdb.287.1216962
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