Breadcrumb
Bureau of Economic Geology Publications
| Title | Publication Year Sort ascending | Abstract | Author | Publisher | |
|---|---|---|---|---|---|
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Upper Franconian and Lower Trempealeauan Cambrian trilobites and brachiopods, Wilberns Formation, central Texas | 1962 | Forty-three species belonging to 28 genera, 12 species of brachipods belonging to 8 genera, and 1 species of gastropods are described from the Morgan Creek, Point Peak, and San Saba Members of the Wilberns Formation in the Llano Uplift. |
Bell, W.C., Ellinwood, H.L. | Bureau of Economic Geology |
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The Hill-Shuler Local Faunas of the Upper Trinity River, Dallas and Denton Counties, Texas | 1962 | The Pemberton Hill-Lewisville (T-2) terrace deposits of the Trinity River in Dallas and Denton Counties are divided into four consecutive members. Sixty-three vertebrates, 32 mollusks, and several insects and plants were collected from 3 members and are discussed in the report. |
Slaughter, B.H., Crook, W.W., Harris, R.K., Allen, D.C. | Bureau of Economic Geology |
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The Mineral Industry of Texas in 1960 | 1961 | Netzeband, F.F., Early, T.R., Girard, R.M. | Bureau of Economic Geology | |
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Texas Gemstones | 1961 | Stones and minerals that are sufficiently beautiful, durable, and rare are known as gemstones. A gemstone with only one of these qualities is less desirable than one with all three. |
King, E.A.,Jr. | Bureau of Economic Geology |
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Stratigraphic Names in the Midway and Wilcox Groups of the Gulf Coastal Plain | 1961 | In the past 100 years, more than 100 names have been used to designate parts or all of the outcropping Midway and Wilcox rocks in the Gulf Coastal Plain; less than half of these names are used currently by Coastal Plain geologists, and the validity of some of the remaining named rock units has be |
Fisher, W.L. | Bureau of Economic Geology |
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Field excursion central Texas -- bentonites, uranium-bearing rocks, vermiculites | 1961 | The departure point of the Villa Capri Motor Hotel may be gone, but the geologic information within Guidebook Number 3 remains relevant to this day: "The four stops of this field trip are in the Upper Eocene (Jackson) and Oligocene volcanic ash and bentonite beds, which crop out about |
Folk, R.L., Hayes, M.O., Brown, T.E., Eargle, D.H., Weeks, A.D., Barnes, V.E., Clabaugh, S.E. | Bureau of Economic Geology |
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The Mineral Industry of Texas in 1959 | 1960 | Netzeband, F.F., Girard, R.M. | Bureau of Economic Geology | |
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Stratigraphy of the Blach Ranch -- Crystal Falls section (Upper Pennsylvanian), northern Stephens County, Texas | 1960 | Three mappable members in the upper part of the Thrifty formation (Blach Ranch limestone, unnamed shale, and Breckenridge limestone), two in the lower part of the overlying Harpersville formation (Quinn clay and Crystal Falls limestone), and six minor lentils, all in the outcropping Cisco group, |
Brown, L.F., Jr. | Bureau of Economic Geology |
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Texas Fossils: An Amateur Collector's Handbook | 1960 | Almost everyone has seen the fossilized remains of prehistoric plants or animals. These might have been the skeleton of a gigantic dinosaur, the petrified trunk of an ancient tree, or the shells of snails or oysters that lived in the great seas that covered Texas millions of years ago. |
Bureau of Economic Geology | |
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Geology of Van Horn Mountains, Texas | 1959 | About 10 miles south of Van Horn, Texas, the Van Horn Mountains rise abruptly above an intermontane plain and extend southward to the Sierra Vieja. The area lies primarily in the southwestern part of Culberson County but extends into Hudspeth and Jeff Davis counties. |
Twiss, P.C. | Bureau of Economic Geology |