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Now showing items 1-8 of 8
Geology of the Applebush Hill area, south Antelope Valley, Nye County, Nevada
(University of Nevada, Reno, 1961)
Lower Paleozoic rocks of an eastern miogeosynclinal assemblage have been mapped and studied in detail in the Applebush Hill area. Their stratigraphic, paleontological, and structural aspects have been correlated to the ...
Geology of the Lantern property near Scossa mining district, Pershing County, Nevada
(University of Nevada, Reno, 1985)
The Lantern property and Scossa mining district o-f northern Pershing County, Nevada, exhibit gold-silver mineralization characteristic o-f epithermal systems. Mineralized boulders deposited as clasts in a mid-Tertiary ...
The geology of the Black Mountain area, Mineral County, Nevada
(University of Nevada, Reno, 1969)
A geologic map of the Black Mountain area has been created. The area is underlain by for intrusive rock bodies. Roof pendants of Triassic(?) metavolcanics, recrystallized limestone, and metamorphosed shallow intrusives are ...
Geology of the Bishop Creek area, Elko County, Nevada
(University of Nevada, Reno, 1968)
The geology and stratigraphy of the Bishop Creek area of Elko County, Nevada, have been studied and a geologic map is presented.
Stratigraphy and structure in the Belmont mining district, Nye County, Nevada
(University of Nevada, Reno, 1975)
The stratigraphy and structure in the Belmont mining district have been investigated. The sediments in the area have been metamorphosed as a result of intrusion. Drag folds are present within the sedimentary rocks and three ...
Stratigraphy, structure, geophysics, and water chemistry of the Jersey Valley area, Pershing and Lander Counties, Nevada
(University of Nevada, Reno, 1981)
The stratigraphy, structure, geophysics, and water chemistry of the Jersey Valley area have been studied. Photogeologic interpretation indicate faults forming grabens within Jersey Valley. Maximum subsurface temperature ...
Geology of the Brock Canyon area, Monitor Range, Eureka County, Nevada
(University of Nevada, Reno, 1965)
Paleozoic rocks within the Brock Canyon area were studied with respect to extending the previously mapped structural and stratigraphic features found in the Antelope Valley and east Monitor Range area.
Stratigraphy, structure and geochemistry of the Horse Canyon disseminated Gold Mine, Eureka Co., Nevada
(University of Nevada, Reno, 1992)
The Horse Canyon gold deposit is hosted by Devonian Wenban Limestone (lower plate), and Ordovician Vivini Formation (upper plate). The Roberts Mountains thrust runs through the deposit.