THE PERMIAN BASIN OF WEST TEXAS AND SOUTHEAST NEW MEXICO: A WORLD-CLASS PETROLEUM PROVINCE
The Permian Basin has a complex geologic history that includes an Early Paleozoic precursor basin (Tobosa Basin). Beginning in latest Mississippian and Early Pennsylvanian time, the Tobosa Basin was tectonically differentiated into a series of basement-involved uplifts and high-standing shelves separated by rapidly-subsiding depressions (Delaware, Val Verde, and Midland basins). Structural differentiation was driven by the assembly of Pangea and development of the Ancestral Rocky Mountain complex as the Permian Basin was located at the SW nexus of Gondwana – Laurentia collision (Marathon – Ouachita fold and thrust belt) and Pacific subduction along the western margin of Laurentia, which drove Ancestral Rocky deformation. Rapid subsidence of the Delaware and Midland basins occurred during the Early Permian as the evolving foredeep was loaded with 10 km or more of sediment. This period of subsidence set in motion the thermal maturation of many of the deeper source rock intervals beginning in Late Permian time. The basin was sealed by Late Permian evaporites and remained relatively stable throughout most of the Mesozoic. Varying amounts of uplift associated with Laramide and Basin and Range tectonism have differentially affected the Permian Basin petroleum systems, more adversely to the west.