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Tectonostratigraphic analysis of Permian Basin subsurface data indicates that earlier-formed faults were reactivated after the Permian. Present-day structure and depositional environments of the Spraberry and San Andres formations provide solid evidence that reactivation was later than the major regional Carboniferous through early Permian deformation.
Laramide, Tectonics, Wasson Field, San Andres, Structure, Permian Basin, Spraberry, Permian, Midland Basin, Fault
Laramide, Tectonics, Wasson Field, San Andres, Structure, Permian Basin, Spraberry, Permian, Midland Basin, Fault
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