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Copyright © 2024. The American Association of Petroleum Geologists. All rights reserved.
DOI:10.1306/01242423080
Interpretation, characterization and slip hazard assessment of faults in the Midland Basin, West Texas, United States
Elizabeth A. Horne, Peter H. Hennings, Katie M. Smye, Amanda Z. Calle, Alan P. Morris, and Guo-Chin Dino Huang
Bureau of Economic Geology, Jackson School of Geosciences, the University of Texas at Austin, Austin, TX, 78758, USA
Ahead of Print Abstract
We map and analyze 795 basement-rooted faults, expressed as high-angle reverse and near-vertical strike-slip faults. High-angle reverse faults that strike NNW-SSE define the eastern margin of the Central Basin platform and generate the greatest structural relief. East of the Central Basin platform, NNW-SSE and NNE-SSW striking reverse faults bound low-amplitude uplifts. Reverse faults are accompanied by WNW-ESE and WSW-ENE striking strike-slip faults, which limit the lateral length of reverse faults and associated uplifts, coinciding with a reversal in fault-bounded uplift vergence direction, and exhibit evidence for transpressional translation. These observations suggest that reverse structures initiated during Late Paleozoic orogenesis, but WNW-ESE and WSW-ENE striking strike-slip faults are the Late Paleozoic reactivation of a long-standing Proterozoic fabric.
Earthquakes have occurred on basement-rooted high-angle reverse and reverse–strike-slip faults, which are reactivated under present-day stress conditions as normal and normal–strike-slip, respectively. FSP analyses show that WNW-ESE and WSW-ENE striking faults are sensitive to reactivation under modest pore pressure increase. Our results provide a foundation to investigate causal behavior, characterize fault slip hazard, and can therefore be used to plan and regulate ongoing petroleum operations.
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