--> Stratigraphy, Seismic Characteristics, and Reservoir Properties of the Desmoinesian Granite Wash, Buffalo Wallow Field Area, Anadarko Basin, Texas

AAPG Annual Convention and Exhibition

Datapages, Inc.Print this page

Stratigraphy, Seismic Characteristics, and Reservoir Properties of the Desmoinesian Granite Wash, Buffalo Wallow Field Area, Anadarko Basin, Texas

Abstract

The Desmoinesian Granite Wash is a productive oil and gas play of the southern Anadarko Basin. It includes a series of alluvial fans, fan-deltas, proximal turbidites, and debris flows deposited in association with the Amarillo-Wichita uplift. The deposits occur as several thousand feet of conglomerates, sandstones, carbonates, and shales that form complex low-permeability and generally low-porosity reservoirs. The stratigraphic and structural framework and reservoir characteristics of the Desmoinesian Granite Wash are established using a 28 mi2 (72 km2) 3-D seismic survey, logs from 450 wells, and petrophysical data derived from published cores. The lithologies and well-log signatures of the different reservoirs are highly variable. The dominant lithofacies include cross-bedded sandstone, parallel-stratified sandstone, planar-laminated sandstone, structureless sandstone, bioturbated sandstone, and silt-rich mudstone. Artificial-neural-network (ANN) techniques are used to estimate lithology logs in non-cored wells by utilizing core and well logs. Key stratigraphic surfaces are commonly related to laterally extensive shales. The Desmoinesian Granite Wash is subdivided into 10 intervals based on net-to-gross ratio, regional trends in well-log signatures, and seismic reflection character. Detailed interpretation of 3-D seismic data also illustrates that the Granite Wash interval exhibits several high-angle reverse faults with significant offset. Results from P-impedance inversion are used with the estimated lithology logs, and the established stratigraphic and structural framework to constrain the spatial distribution of lithology and petrophysical properties in 3-D reservoir models. The models illustrate the stratigraphic architecture, main structural elements, and their relationship to Granite Wash reservoir quality distribution for the study area.