Rock property and seismic attribute analysis of a chert reservoir in the Devonian Thirtyone Formation, West Texas, U.S.A.
Rock property and seismic attribute analysis of a chert reservoir in the Devonian Thirtyone Formation, West Texas, U.S.A.
Geophysics (September 2006) 71 (5): B151-B158
- acoustical properties
- anticlines
- body waves
- cartography
- chemically precipitated rocks
- chert
- Crane County Texas
- Devonian
- elastic waves
- folds
- fractures
- geophysical methods
- geophysical surveys
- impedance
- lithofacies
- oil and gas fields
- P-waves
- Paleozoic
- petroleum
- petroleum exploration
- porosity
- prediction
- production
- reservoir properties
- reservoir rocks
- sedimentary rocks
- seismic attributes
- seismic methods
- seismic waves
- structural traps
- surveys
- systems
- Texas
- Thirtyone Formation
- traps
- United States
- West Texas
- University Waddell Field
In west Texas, fractured-chert reservoirs of Devonian age have produced more than 700 million barrels of oil. About the same amount of mobile petroleum remains in place. These reservoirs are characterized by microporosity; they are heterogeneous and compartmented, which results in recovery of less than 30% of the oil in place. In this case study the objective was to use cores, petrophysical logs, rock physics, and seismic attributes to characterize porosity and field-scale fractures. The relations among porosity, velocity, and impedance were explored and also reactions among production, impedance, and lineaments observed in 3D attribute volumes. Laboratory core data show that Gassmann's fluid-substitution equation works well for microporous tripolitic chert. Also, laboratory measurements show excellent linear correlation between P-wave impedance and porosity. Volumetric calculations of reflector curvature and seismic inversion of acoustic impedance were combined to infer distribution of lithofacies and fractures and to predict porosity. Statistical relations were established between P-wave velocity and porosity measured from cores, between P-wave impedance and producing zones, and between initial production rates and seismic "fracture lineaments". The strong quantitative correlation between thick-bedded chert lithofacies and seismic impedance was used to map the reservoir. A qualitative inverse relation between the first 12 months of production and curvature lineaments was documented.