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Crustal structure of the Texas gulf coast
(Texas Tech University, 1973-05)
The coastal region of Texas is a zone of transition from oceanic structure in the Gulf of Mexico to continental structure in central Texas. Knowledge of crustal structure
in this region is necessary to understand the ...
Crustal xenoliths from Potrillo Maar: Implications for evolution of continental crust beneath the southern Rio Grande rift
(Texas Tech University, 2003-08)
The mid-crustal xenoliths from Potrillo maar record a petrologic and geochemical history that has until now been unknown from the Potrillo volcanic field. The igneous and meta-igneous xenoliths are samples of one or more ...
Sediments and Topography of the Western Gulf of Mexico
(Texas Tech University, 1967-08)
Relative frequencies of temperature sensitive planktonic foraminifera, in sediment cores raised from the continental slope and Sigsbee Abyssal Plain in the Gulf of Mexico, indicate alternating periods of warm and cold ...
The structural and metamorphic history of the Oakhurst roof pendant, Mariposa and Madera Counties, California
(Texas Tech University, 1972-12)
The Oakhurst roof pendant, near Oakhurst, California, consists of three pre-Cretaceous clastic metasedimentary rock units, surrounded and intruded by rocks of the Sierra Nevada batholith. Two zones of probable "sheared ...
Depositional dynamics of the Brushy Canyon Formation, Delaware Basin, Texas
(Texas Tech University, 1966-05)
The Brushy Canyon Formation, lowermost of the DeLaware Mountain Group, represents a network of submarine channel and overbank deposits, The site of deposition, the Delaware basin, was analogous to present deep basins off ...
Descriptive geometry in the geosciences
(Texas Tech University, 1952-06)
Not available
Crustal structure of the central High Plains of Texas from Rayleigh wave dispersion
(Texas Tech University, 1972-12)
Not Available.
Cenozoic stratigraphy and geomorphology of Lynn and Terry counties, Texas.
(Texas Tech University, 1975-08)
Not available
Structural relationships and chronologies of two chert to clastic rock successions, Western Sierra Nevada, California
(Texas Tech University, 1976-08)
In the western Sierra Nevada, California, an east to west rock succession of layered chert, pelitic-siliceous rock, and fine-grained clastic rock characterizes part of the Paleozoic Calaveras Formation. Along the Merced ...