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Abstract

Prentice field is a narrow stratigraphic trap of Permian age, formed by an updip porosity pinch out at a paleo shelf edge on the Northwest shelf of the Midland Basin, North Texas, U.S.A.. The reservoir section consists predominately of dolomitized mudstones, packstones and grainstones with abundant anhydrite, and a few intercalations of dolomite cemented silt store beds (< 5%). The facies grade from inter tidal to subtidal environments with high frequency fluctuations.

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/content/papers/10.3997/2214-4609.201411830
1993-06-08
2024-03-29
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201411830
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