University of Nevada, Reno
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Structural control of mineralization at the Aurora mining district, Mineral County, Nevada
(University of Nevada, Reno, 1964)
No abstract provided.
The geology of the Bovard mining district, Gabbs Valley Range, Mineral County, Nevada
(University of Nevada, Reno, 1982)
The Bovard Mining District, located in the Gabbs Valley Range, Mineral County, Nevada produced about $360,000.00 in gold and silver. The mineralization is of the epithermal vein type. The district is underlain by a thick ...
Geology and alteration of the Wedekind and part of the Peavine districts, Washoe County, Nevada
(University of Nevada, Reno, 1977)
The geology and alteration of the Wedekind and part of the Peavine Districts were studied. Island arc rocks are intruded by Sierran granitic rocks and are overlain by magmatic arc volcanics. The Peavine and Wedekind Districts ...
Geology, alteration, and mineralization at Hasbrouck Mountain, Divide district, Esmeralda County, Nevada
(University of Nevada, Reno, 1985)
The geology, alteration, and mineralization at Hasbrouck Mountain were studied.
Geology and mineralization of the Lucky Hill pit, Candelaria mine, Mineral County, Nevada
(University of Nevada, Reno, 1988)
The geology and mineralization of the Lucky Hill Pit was studied.
Geology and mineralization of the Marietta area, Mineral County Nevada
(University of Nevada, Reno, 1978)
Pre-Tertiary layered rocks dominate the study area at Marietta, Nevada, in the central Excelsior Mountains. In stratigraphic order these include andesite volcanics and volcaniclastic sediments, calcareous siltstone, ...
Geology of the Buffalo Valley prospect, Lander County, Nevada
(University of Nevada, Reno, 1985)
No abstract provided.
Geology and ore deposits of Sand Springs district, Churchill County, Nevada
(University of Nevada, Reno, 1980)
The geology and structure of the Sand Springs mining district is studied and described.
The origin of crystalline magnesite deposits
(University of Nevada, Reno, 1958)
The origin of crystalline magnesite deposits has been investigated. Magnesite deposits formed by hydrothermal or replacement processes are extremely rare.
The petrology of a zoned granitic stock, Stillwater Range, Churchill County, Nevada
(University of Nevada, Reno, 1975)
The petrology of a zoned granitic stock located in the Stillwater Range of Churchill County, Nevada, has been studied.