Abstract:The Morrow-Springer pressures in the Anadarko Basin have become a major factor in the exploration and exploitation of the Basin's major pre-Permian gas reserve. The tectonics affecting the Morrow-Springer formations during and after deposition of the sediments may be partly responsible for the abnormally low and high pressures in their respective areas. Isopach maps of the Morrow-Spriinger indicate the major divisions of pressure gradient in the formations. BHP gradient maps can be interpreted in areas where c… Show more
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