Breadcrumb
Bureau of Economic Geology Publications
Title | Publication Year Sort ascending | Abstract | Author | Publisher | |
---|---|---|---|---|---|
![]() |
Recognition of Hipparions and other horses in the middle Miocene Mammalian faunas of the Texas Gulf region | 1952 | New information concerning the ancestry of the later Tertiary horses, Calippus, Protohippus (in the original sense), Hipparion, Neohipparion, and Nannippus, has been obtained from a restudy of the various mammalian farmas of the Coastal Plain in Texas, based in the main on the extensive collectio |
Quinn, J.H. | Bureau of Economic Geology |
![]() |
Agua Fria quadrangle, Brewster County, Texas | 1951 | Moon, C.G. | Bureau of Economic Geology | |
![]() |
Pegmatites of the Van Horn Mountains, Texas | 1951 | Zoned and unzoned perthite-quartz-plagioclase-muscovite pegmatites in the form of tabular bodies, irregular bodies with tabular branches, irregular masses, elongate lenses, lit-par-lit zones, and small augen and stringers are distributed throughout the Precambrian metasedimentary rocks of the Mic |
Flawn, P.T. | Bureau of Economic Geology |
![]() |
Buried Hill at Wilcox-Carrizo Contact in East Texas | 1951 | A recently discovered buried hill, at least 77 feet high, is composed of strata of the Wilcox group (lower Eocene) and covered on its flanks by cross-bedded sands of the lower Carrizo and at the top by level-bedded shales and silts of the upper Carrizo formation. |
Stenzel, H.B. | Bureau of Economic Geology |
![]() |
Geologic map and structure sections of the Christmas and Rosillos Mountains, Brewster County, Texas | 1951 | Bloomer, R.R. | Bureau of Economic Geology | |
![]() |
Subsurface Woodford black shale, West Texas and southeast New Mexico | 1950 | The geographic distribution, lithology, thickness, and paleontology of the subsurface Woodford in the Permian basin are described and illustrated. |
Ellison Jr., S.P. | Bureau of Economic Geology |
![]() |
Geology of the Barrilla Mountains, Texas | 1950 | The Barrilla Mountains, in the northeastern part of the Davis Mountains of Trans-Pecos Texas, are composed of Tertiary volcanic materials. Five tuffs and five lava flows, 1500 feet thick occurring throughout the mountains, persist in thickness and lithologic characteristics. |
Eifler, G.K. | Bureau of Economic Geology |
![]() |
Successional Speciation in Paleontology: The Case of the Oysters of the Sellaeformis Stock | 1949 | The successional mode of speciation of Julian Huxley (1942) may be defined as gradual transformation of one species into a successor species, or several of them, during the course of geologic time without primarily involving geographic, ecologic, or adaptive segregation. |
Stenzel, H.B. | Bureau of Economic Geology |
![]() |
Correlation of gravity observations with the geology of the Coal Creek serpentine mass, Blanco and Gillespie Counties, Texas | 1949 | Gravitational observations were made of the pre-Cambrian Coal Creek serpentine mass in Blanco and Gillespie Counties, Texas, the geology of which had been mapped previously. |
Romberg, Frederick, Barnes, V.E. | Bureau of Economic Geology |
![]() |
Iron ore in the Llano region, central Texas | 1949 | The magnetic iron-ore prospects of the Llano region of central Texas were investigated in a program which combined dip-needle and gravity-meter surveys by the Bureau of Economic Geology of The University of Texas and the U.S. Geological Survey with exploration by the U.S. Bureau of Mines. |
Barnes, V.E., Goldich, S.S., Romberg, Frederick | Bureau of Economic Geology |