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Title: Clay mineralogy and depositional history of the Frio Formation in two geopressured wells, Brazoria County, Texas

Conference ·
OSTI ID:5053149

Twenty-three shale samples ranging in depth from 5194 ft to 13,246 ft from Gulf Oil Corporation No. 2 Texas State Lease 53034 well and 33 shale samples ranging in depth from 2185 ft to 15,592 ft from General Crude Oil Company/Department of Energy No. 1 Pleasant Bayou well were examined by x-ray techniques to determine the mineralogy of the geopressured zone in the Brazoria Fairway. Both wells have similar weight-percent trends with depth for a portion of the mineralogy. Calcite decreases, and plagioclase, quartz and total clay increase slightly. Within the clays, illite in mixed-layer illite/smectite (I/S) increases and smectite in mixed-layer I/S decreases. Four minerals have distinctly different trends with depth for each well. In the No. 2 Texas State Lease 53034 well, potassium feldspar and mixed-layer I/S decrease, kaolinite increases, and discrete illite is constant. In the No. 1 Pleasant Bayou well, potassium feldspar and kaolinite are constant, mixed-layer I/S increases, and discrete illite decreases.

Research Organization:
Trinity Univ., San Antonio, TX (USA)
DOE Contract Number:
AC08-79ET27111
OSTI ID:
5053149
Report Number(s):
CONF-821009-1; ON: DE82016166
Resource Relation:
Conference: 32. annual meeting of the Gulf Coast Association of Geological Societies, Houston, TX, USA, 26 Oct 1982
Country of Publication:
United States
Language:
English