Now showing items 1-5 of 5
The use of Fe/Mn oxide-rich fracture coatings in the geochemical exploration for precious metal deposits, a comparison with standard rock and soil geochemistry
(University of Nevada, Reno, 1982)
Research indicates that the use of Fe/Mn oxide-rich fracture coatings as a geochemical medium for precious metals exploration is scientifically valid.
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.
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.
Geology, trace element geochemistry and hydrothermal alteration at the Buckhorn gold mine, Eureka County, Nevada
(University of Nevada, Reno, 1987)
Precious-metal mineralization is hosted in a sequence of Tertiary volcanic and sedimentary rocks. The mineralization was deposited by a paleo-hot spring system.
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. ...