Contents
Preface
Textures, Mineralogy, and Reservoir Properties of an Altered Mafic Tuff Core from the Upper Cretaceous (Lower Campanian) of Central Texas
Robert M. Reed and Robert G. Loucks
Depositional Systems, Lithofacies, and Lithofacies Stacking Patterns of the Jurassic Smackover Formation (Oxfordian) and Buckner Anhydrite (Kimmeridgian) in Van Zandt County, Texas: A Type-Cored Section from Northeastern Texas
Peter Schemper, Robert G. Loucks, and Qilong Fu
Depositional Systems, Lithofacies, and Reservoir Characterization of the Upper Cretaceous Austin Chalk, Brookeland and Burr Ferry Fields in East Texas and Western Louisiana
Robert G. Loucks, Sheng Peng, Kelly E. Hattori, Priyanka Periwal, Josh R. Lambert, Christopher K. Zahm, and Lucy T. Ko
The Early Cretaceous Transition from Carbonate to Siliciclastic Deposition in the Deep Waters of the Northern Gulf of Mexico: New Insights from the Keathley Canyon 102 #1 Well
Michael L. Sweet, Marcie Purkey Phillips, Robert Cunningham, John W. Snedden, and Ryan Weber
Preliminary Source Rock Evaluation of the Lower Cenozoic Toledo Formation, Belize Basin, Southern Belize
Jason D. Fisher and David T. King, Jr.
Outcrop Evidence for Variations in Channel-Floodplain Facies and Stratal Architectures across the Simsboro to Calvert Bluff Transition, Wilcox Group, Butler, Texas
Peter P. Flaig, Christopher N. Denison, William A. Ambrose, and Thomas D. Demchuk
Influence of Stratigraphic Modeling Scales on Shale Oil Resources Assessment of the Midland Basin
Robin Dommisse
Barremian-Albian Larger Benthic Foraminiferal Zones (Lower Cretaceous), Gulf of Mexico Region: A Key to Correlating Carbonate Reservoirs
Robert W. Scott
The Lower Cretaceous Hensel–Glen Rose Stratigraphic Couplet in the Llano Uplift, Central Texas
Peter R. Rose |
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2022 (Vol. 11)
Cover: Thickness of the Hensel–Glen Rose stratigraphic couplet, Llano Uplift and adjacent areas, Central Texas, showing traces of geologic cross-sections A–A’, B–B’, C–C’, and D–D’. Note that local darkening of thickness colors exists due to the partial-transparent overlay of greyscale tones related to Paleozoic and Precambrian outcrop areas. Contour interval is 50 ft. For more information, please see Rose paper herein. |
