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The AAPG/Datapages Combined Publications Database

AAPG Bulletin

Abstract


Volume: 10 (1926)

Issue: 9. (September)

First Page: 877

Last Page: 884

Title: The Geologic Structure of a Portion of the Glass Mountains of West Texas

Author(s): Philip B. King

Abstract:

In the Glass Mountains of west Texas a thick section of marine Permian rocks is exposed. It rests unconformably upon strongly folded Pennsylvanian and early Paleozoic rocks and is unconformably overlaid by Comanchean beds. The regional structure is a northwest dip of from 5° to 15°. Minor structures consist of some northwest trending faults of short length, but locally with considerable throw. It is concluded that these structures are of post-Comanchean age and that a little more than half the deformation in the mountains took place at that time. The pre-Comanchean folding consists of a northwest-dipping monocline upon which are minor arches whose relationship to the later anticlines is of an erratic nature.

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