Breadcrumb
Bureau of Economic Geology Publications
| Title | Publication Year Sort ascending | Abstract | Author | Publisher | |
|---|---|---|---|---|---|
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The geologic story of Longhorn Cavern | 1963 | Bureau of Economic Geology | ||
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Field excursion - geology of Llano region and Austin area | 1963 | Barnes, V.E., Bell, W.C., Clabaugh, S.E., Cloud, P.E., Jr., Young, Keith, McGehee, R.V. | Bureau of Economic Geology | |
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Pleistocene geology of Red River basin in Texas | 1963 | The Red River rises in northeastern New Mexico and extends across northern Texas and east of the Panhandle serves as the northern border of that State. The late Cenozoic geology of the Red River basin has been studied intensively in northwestern Texas and in Louisiana. |
Frye, J.C., Leonard, A.B. | Bureau of Economic Geology |
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Lignites of the Texas Gulf coastal plain | 1963 | One of the basic mineral resources of Texas is abundant deposits of lignite in Eocene rocks of the Gulf Coastal Plain. |
Fisher, W.L. | Bureau of Economic Geology |
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Geologic map of Southeastern Llano Uplift, Llano, Burnet, Blanco, and Gillespie counties, Texas | 1963 | McGehee, R.V. | Bureau of Economic Geology | |
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The Mineral Industry of Texas in 1962 | 1963 | Netzeband, F.F., Early, T.R., Girard, R.M. | Bureau of Economic Geology | |
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Geology of the Johnson City Quadrangle, Blanco County, Texas | 1963 | Barnes, V.E. | Bureau of Economic Geology | |
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Geology of the Eagle Mountains and Vicinity, Hudspeth County, Texas | 1963 | Eagle Mountains and vicinity include three physiographically distinct but stratigraphically and structurally related sub-units: a central, topographically high mesa, Eagle Mountains; a much lower northwestward extension, Devil Ridge; and a south-southeastward extension, Indio Mountains. |
Underwood, J.R. | Bureau of Economic Geology |
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Correlation of Cambrian Rocks in Central Texas | 1963 | Barnes, V.E. | Bureau of Economic Geology | |
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Pleistocene molluscan faunas and physiographic history of Pecos Valley in Texas | 1962 | Studies of physiographic relations and of fossil molluscan faunas made in the Pecos River valley region (Val Verde County to the Texas�New Mexico border) reveal extensive, well-pedimented surfaces southwest of the river extending from the Davis Mountains to near the present channel. |
Leonard, A.B., Frye, J.C. | Bureau of Economic Geology |