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Abstract
UPPER PERMIAN TO PLIOCENE, SAN ANGELO AREA, TEXAS, 1961
Pages 50-53
Origin of Siliceous Dockum Conglomerates
Robert Roth
Abstract
A fossiliferous chert shingle discovered in a Dockum outlier in Motley County, Texas, contained fusulinids which apparently came from the Hueco, Franklin, or Glass mountains of West Texas. A suite of Dockum pebbles was collected from this outlier and a megascopic and microscopic examination indicated a source near the Marathon uplift, a distance of at least 300 miles.
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