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Now showing items 1-7 of 7
Geology and mineral deposits of the Pyramid district, southern Washoe County, Nevada
(University of Nevada, Reno, 1975)
The Pyramid district is thirty miles north-northeast of Reno, Nevada in the northern Pah Rah Range. Known mineralization in the district is confined to west and northwest trending veins along fracture zones and faults ...
Geological applications of remote sensing in the Virginia Range, Nevada
(University of Nevada, Reno, 1988)
The geology of the Virginia Range was studied using remote sensing techniques. The research shows the capabilities of various remote sensing systems to discriminate and map hydrothermal alteration mineral assemblages, and ...
Studies of silicic volcanic geology and geochemistry in the Great Basin of western North America
(University of Nevada, Reno, 1995)
This dissertation addresses several aspects of volcanic and structural geology in Oasis Valley and the Bullfrog Hills near the Timber Mountain caldera complex.
The calera vein system, Orcopampa District, southern Peru: association of tectonism, magmatism and hydrothermal activity in the formation of a bonanza Ag-Au deposit
(University of Nevada, Reno, 1992)
The tectonism, magmatism, and hydrothermal activity of the Calera vein system was studied.
The stratigraphy, petrology, and paleomagnetics of the Moss Flat area, Lake County, Oregon
(University of Nevada, Reno, 1981)
The stratigraphy, petrology, and paleomagnetics of the Moss Flat area of Lake County, Oregon, have been studied. The area consists of a Miocene ash-flow tuff sequence which has been correlated to the Upper Cedarville Series ...
Alteration and geochemical characteristics of the upper parts of selected porphyry systems, western Nevada
(University of Nevada, Reno, 1983)
The alteration and geochemical characteristics of the upper parts of selected porphyry systems located in western Nevada were studied.
Geology of the Puzzle vein, Creede mining district, Colorado
(University of Nevada, Reno, 1970)
The geology of the Puzzle Vein, located in the Creede mining district, has been studied. The Puzzle vein is conceptually an epithermal precious metal vein dominantly composed of layered barite formed by fissure filling. ...