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Permian (Guadalupian) shelf deposition and diagenesis: Tansill Formation of Cheyenne field, Winkler County, Texas

Conference · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:7084831
Cheyenne field, Winkler County, Texas, produces oil from shelf-margin lithofacies of the Tansill Formation of late Guadalupian age. The Tansill Formation encountered in the Cheyenne field compares favorably with basin-margin outcrops found in the Guadalupe Mountains of New Mexico and Texas. The Cheyenne field reservoir exhibits varied lithologies and porosities in the Tansill Formation. Fresh-water phreatic diagenesis created moldic porosity in the outer shelf, green-algal lithofacies. Fresh-water vadose conditions existed during low sea level stands preserving intergranular porosity in the pisolitic lithofacies of the shelf-crest tepee complex. Fresh-water vadose diagenesis also helped form burrow-moldic porosity and fenestral porosity in the inner shelf peloidal lithofacies. Periodic hypersaline vadose conditions occluded some porosity with evaporites and aragonitic cements. Dolomitization of the Tansill Formation occurred in the mixing zone between a seasonal fresh-water lens in the shelf-crest sediments and the saline water of the Permian sea and inner shelf lagoon. Porosity is best developed in the thin beds of the outer shelf, green-algal lithofacies. The arid climate at the time of deposition was essential in maintaining porosity created by early diagenesis and for the absence of abundant vadose cements in the Tansill Formation. The trap in Cheyenne field is depositionally controlled by updip, nonporous, and impermeable sediments of the inner shelf lagoon. Anhydrites of the overlying Salado Formation provide an excellent seal.
Research Organization:
Union Oil Co., Casper, WY
OSTI ID:
7084831
Report Number(s):
CONF-840297-
Conference Information:
Journal Name: Am. Assoc. Pet. Geol., Bull.; (United States) Journal Volume: 68:1
Country of Publication:
United States
Language:
English