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Now showing items 41-50 of 222
Geology at Tungsten, Nevada, emphasizing structural aspects
(University of Nevada, Reno, 1957)
Contact-metamorphic deposits containing scheelite are found at Tungsten, Pershing County, Nevada. Upper Triassic limestone beds were replaced by emanations from granodiorite stocks, forming tactite deposits bearing tungsten. ...
Geology of the Nevada Scheelite Mine, Mineral County, Nevada
(University of Nevada, Reno, 1982)
The Nevada Scheelite area is underlain by a Mesozoic sequence of volcanic, volcanoclastic, and carbonate rocks of Jurassic-Triassic age, in part correlative with the Middle Triassic Luning Formation of west- central ...
A geochemical study of the barite deposits of Mineral County, Nevada
(University of Nevada, Reno, 1973)
The barite deposits of Mineral County, Nevada are localized along the intersection of the Walker Lane and the Antler Orogenic belts. There are two distinct types of barite deposits within Mineral County, bedded deposits ...
Geology of the Mound House area, Ormsby and Lyon Counties, Nevada
(University of Nevada, Reno, 1961)
An area of approximately 32 square miles was mapped in the vicinity of Mound House, an abandoned railroad siding between Carson City and Dayton, Nevada. The oldest rocks exposed are Mesosoic metasedimentary and meta-igneous ...
Underground mining operations at Ruth, Nevada, 1951-1958
(University of Nevada, Reno, 1958)
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Structural, tectonic and Quaternary study of the eastern Madeline Plains, California and southwestern Smoke Creek Desert, Nevada
(University of Nevada, Reno, 1990)
A structural, tectonic and Quaternary study of the eastern Madeline Plains (MP) and southwestern Smoke Creek Desert (SCD) in northeastern California and northwestern Nevada indicates that: 1) the Likely fault zone (LFZ) ...
Arsenic as an indirect geochemical guide to epithermal precious metal deposits
(University of Nevada, Reno, 1963)
No Abstract Provided
The geology of a part of the Olinghouse mining district, Washoe County, Nevada
(University of Nevada, Reno, 1980)
The geology of a part of the Olinghouse mining district was studied. Igneous rocks are primarily found in the area.
Quantitative analysis of groundwater flow in valley-fill deposits in Steptoe Valley, Nevada
(University of Nevada, Reno, 1985)
Groundwater flow in Steptoe Valley in east-central Nevada was analyzed with the aid of a steady-state groundwater flow model.
Preliminary analysis of the physical stratigraphy, depositional environment, and paleoecology of the Miocene non-marine deposits, Stewart Valley, Nevada
(University of Nevada, Reno, 1986)
The physical stratigraphy, depositional environment and paleoecology of the Late Tertiary lake beds of Stewart Valley were studied. The sediments display a record of changes in depositional rates, lake level fluctuation, ...