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U.S. Department of Energy
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Factors controlling geopressured geothermal reservoir quality--Frio sandstone facies, Texas Gulf Coast

Conference ·
OSTI ID:7369245

Geopressured geothermal reservoir quality along the Texas Gulf Cioast is controlled by sandstone depositional environment, mineralogical composition, and consolidation history (compaction, cementation, and leaching). The best Frio reservoirs occur at the top of deltaic progradational sequences in distributary-mouth bar and distributary-channel sandstone facies. Poor reservoir quality characterizes proximal delta front and distal delta front sandstones. Sandstone mineralogical composition varies from quartzose feldspathic volcanic litharenite and quartzose lithic arkose along the upper Texas Gulf Coast to feldspathic volcanic litharenite rich in carbonate rock fragments along the lower Texas Gulf Coast. The four major stages of consolidation of Frio sandstones are discussed. Geothermal reservoirs are not composed of simple primary porosity between grains, but rather consist of secondary leached porosity. Austin Bayou Prospect in Brazoria County, Texas, is a prospective geothermal reservoir that is the product of secondary leached porosity.

Research Organization:
Univ. of Texas, Austin
OSTI ID:
7369245
Report Number(s):
CONF-771153-P1-10
Country of Publication:
United States
Language:
English