--> Abstract: Structural/Stratigraphic Reconstruction of Frontal "Choctaw" Triangle Zone Within Oklahoma Atoka Trend: Early Controls (Prethrusting) on Deposition of Deep-Water Clastic Reservoirs, by D. Cox and R. Foshee; #90989 (1993).
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COX, DAN, Consulting Geophysicist, Carthage, TX, and RON FOSHEE, Seagull Mid-South Inc., Shreveport, LA

ABSTRACT: Previous HitStructuralNext Hit/Stratigraphic Reconstruction of Frontal "Choctaw" Triangle Zone Within Oklahoma Atoka Trend: Early Controls (Prethrusting) on Deposition of Deep-Water Clastic Reservoirs

A Previous HitstructuralNext Hit and stratigraphic study in southwestern Oklahoma, encompassing approximately 30 townships in Atoka, Coal, and Pittsburg counties, was done using several hundred wells, surface geologic Previous HitmapsNext Hit, and more than 400 mi of 1980 seismic data. Isopach Previous HitmapsNext Hit of six Atokan sands covered various areas, all within a deep-water fan setting. Previous HitStructuralNext Hit balancing, done on numerous geologic Previous HitcrossNext Hit Previous HitsectionsNext Hit of six mi or less, allowed correlation of logs of the various reservoirs and Previous HitstructuralNext Hit details within the frontal "Choctaw" triangle zone. Two regional Previous HitcrossNext Hit Previous HitsectionsNext Hit were made based, respectively. on 12 and 16 mi of recent high-fold common-depth-point seismic lines, with a minimum of one-well-per-mile control, diameter data, and surface geology. These Previous HitcrossNext Hit Previous HitsectionsNext Hit were reconstructed by line balancing to illustrate the amount of thrusting in the section and the pre-Pennsylvanian normal faulting that subtly controlled the Atoka sands depositional framework. The thickest and most channelized sands are found downthrown to these earlier faults, with this past relationship now obscured by post-Atokan thrusting.

AAPG Search and Discovery Article #90989©1993 GCAGS and Gulf Coast SEPM 43rd Annual Meeting, Shreveport, Louisiana, October 20-22, 1993.