Publications tagged with Chinati Mountains
| Title | Publication Year Sort ascending | Abstract | Author | Series | Publisher | |
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Geology of the Infiernito caldera and magmatic evolution of the Chinati Mountains, Trans-Pecos Texas | 1992 | The 37-Ma-old Infiernito caldera of the northern Chinati Mountains is a major eruptive center of the mid-Tertiary volcanic field of Trans-Pecos Texas. Volcanism in the Chinati Mountains began with eruption of a sequence of rhyolitic to trachytic lavas, the precollapse lavas. |
Henry, C.D., Price, J.G., Duex, T.W., James, E.W. | Report of Investigations | Bureau of Economic Geology |
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Oligocene volcanism and multiple caldera formation in the Chinati Mountains, Presidio County, Texas | 1983 | The Chinati Mountains caldera, which lies in Trans-Pecos Texas in the southern Basin and Range Province, was formed by eruption of the Mitchell Mesa Rhyolite. |
Cepeda, J.C., Henry, C.D. | Report of Investigations | Bureau of Economic Geology |
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Calderas and mineralization: volcanic geology and mineralization in the Chinati caldera complex, Trans-Pecos Texas | 1981 | This report describes preliminary results of an ongoing study of the volcanic stratigraphy, caldera activity, and known and potential mineralization of the Chinati Mountains area of Trans-Pecos Texas. Many ore deposits are spatially associated with calderas and other volcanic centers. |
Duex, T.W., Henry, C.D. | Geological Circular | Bureau of Economic Geology |
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Mineral deposits in the west Chinati stock, Chinati Mountains, Presidio County, Texas | 1972 | The West Chinati stock, well exposed in San Antonio Canyon and immediately westward on slopes of the southwestern part of the Chinati Mountains, Presidio County, Texas, is a large stocklike body of porphyritic hornblende granite cut by numerous dikes and irregular-shaped plutons of rhyolite, rhyo |
McAnulty, W.N. | Geological Circular | Bureau of Economic Geology |