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AAPG Bulletin

Abstract

AAPG Bulletin, V. 101, No. 4 (April 2017), P. 465-474.

Copyright ©2017. The American Association of Petroleum Geologists. All rights reserved.

DOI: 10.1306/011817DIG17025

Guadalupe Mountains, West Texas and New Mexico: Key excursions

Charles Kerans,1 Chris Zahm,2 Beatriz Garcia-Fresca,3 and Paul (Mitch) Harris4

1Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, 1 University Station C1100, Austin, Texas 78712-0254; [email protected]
2Bureau of Economic Geology, Jackson School of Geosciences, University of Texas at Austin, 1 University Station C1100, Austin, Texas 78712-0254; [email protected]
3Statoil, 6300 Bridge Point Pkwy, Building 2, Suite 100, Austin, Texas 78730; [email protected]
4CSL - Center for Carbonate Research, Department of Marine Geosciences, University of Miami, 4600 Rickenbacker Causeway, Miami, Florida 33149; Department of Earth Science, Rice University, 6100 Main Street, MS 126, Houston, Texas 77005; [email protected]

ABSTRACT

The carbonate and siliciclastic outcrops of the Guadalupe Mountains in the Permian Basin of West Texas and New Mexico have provided a rich set of basic and advanced conceptual models for geologists across the entire spectrum of experience for carbonate-ramp and steep-rimmed–platform settings as well as the adjacent deep-water siliciclastics not dealt with here. Fundamental questions regarding the scale and continuity of reservoir pay facies, the depositional patterns and profiles of shelf-to-slope clinoforms, the width of facies tracts on ramps and rimmed platforms, the distribution and internal composition of reef complexes, the link between reef development and slope depositional patterns, styles of early and late diagenesis including dolomitization and karstification, and structural patterns can all be addressed in the Guadalupe Mountains exposures.

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