--> Abstract: Relationships between Cement, Rock Fabric, Porosity and Permeability, Lower Vicksburg Formation, McAllen Ranch Field, South Texas, by J. D. Grigsby and R. P. Langford; #91004 (1991)
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Relationships between Cement, Rock Fabric, Porosity and Previous HitPermeabilityNext Hit, Lower Vicksburg Formation, McAllen Ranch Field, South Texas

GRIGSBY, JEFFRY D., and RICHARD P. LANGFORD, University of Texas at Austin, Austin, TX

Detailed petrographic mapping of cement distribution, combined with sedimentologic description and petrophysical data, is a powerful technique for describing distribution of reservoir properties. Two cores from the lower Vicksburg Formation, McAllen Ranch field, south Texas, indicate that porosity and Previous HitpermeabilityNext Hit, which vary over several orders of magnitude, are related to a complex interplay between centimeter-scale cement variations, grain size, sedimentary structures, and the development of secondary porosity (dissolution of feldspars and unstable lithic fragments).

Porosity and Previous HitpermeabilityNext Hit plugs in combination with thin section analysis, taken every 5 cm through several representative intervals, reveal the complex controls on reservoir properties. For example, within an upward-coarsening interval a strong relationship exists between grain size, the development of secondary porosity, and Previous HitpermeabilityNext Hit. The coarsest sands of the interval are cemented by quartz overgrowths and variable amounts of calcite. The preferential development of secondary porosity in this "band" results in an average Previous HitpermeabilityNext Hit of 0.169 md. In contrast, as grain size decreases, calcite cementation increases, resulting in a decrease in the development of secondary porosity and an average Previous HitpermeabilityNext Hit of 0.008 md. When chlorite is the predominant cement, Previous HitpermeabilityNext Hit is dep ndent on the development of secondary porosity and is independent of grain size. Within a chlorite-cemented interval, with a relatively constant measured porosity of 16.6 (plus or minus 1)%, Previous HitpermeabilityNext Hit ranged from 0.026 md to 0.372 md. Secondary porosity ranged from 1.5% to 5.5% over this same interval. These variations, which occur in distinct bands in core, result in a complex but predictable distribution in porosity and Previous HitpermeabilityTop.

 

AAPG Search and Discovery Article #91004 © 1991 AAPG Annual Convention Dallas, Texas, April 7-10, 1991 (2009)