Henry F. Schreiner
Angelo State University, San Angelo, TX
Activity
2009
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DAGGER MOUNTAIN, BIG BEND NATIONAL PARK, WEST TEXAS DOES NOT OVERLIE A LACCOLITH
T40 The Mesozoic and Cenozoic Tectonic Evolution of Northwestern Mexico and the Southwestern United States (Posters)Sunday, 18 October 20099:00 AM - 6:00 PMHall A
2008
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Folding on the Flanks of the Southernmost Laramide Uplift, Big Bend Region, Texas
T342 Recent Advances in the Study of the Laramide Orogeny and Related Processes in Mexico and the Southern United StatesThursday, 9 October 20088:00 AM - 12:00 PM