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Reference 3351

Gilluly, James; Masursky, Harold (1965) U. S. Geological Survey Bulletin, Report: B 1175, 117 pp., 1965

AuthorsGilluly, James; Masursky, Harold
Year1965
SourceU. S. Geological Survey Bulletin, Report: B 1175, 117 pp., 1965
Pages117 pp.
PublisherU. S. Geological Survey, Reston, VA, United States USA
ISSN8755-531X
GeoRef1965-018945
Keywordsaeromagnetic; areal geology; Bouguer gravity; Cenozoic; Cortez quadrangle; economic geology; faults; geologic; maps; Mesozoic; metal ores; Nevada; overthrust; Paleozoic; polymetallic ores; Roberts thrust; stratigraphy; United States; USGS

Abstract

The stratigraphy, structure, and economic geology of the Cortez quadrangle, in north-central Nevada, are discussed. The area is of particular interest because of the formerly active bonanza silver cap at Cortez and because of the exposure of the Roberts thrust, one of the great structures of the Cordillera and critical to an understanding of Cordilleran evolution. Paleozoic, Mesozoic, and Cenozoic strata and Tertiary volcanics are exposed in the area. The Roberts thrust is latest Devonian or Early Mississippian in age. Basin and Range faults originated in Pliocene and have been active in post-Pleistocene. Major polymetallic sulfide ores at Cortez are chiefly manto deposits in the Hamburg Dolomite, although large tonnages have been obtained from fissure veins associated with quartz porphyry dikes.

15 samples from this reference

SampleRock nameMajorTraceIsotope
1Tuff yesyes
2Tuff yesyes
3Tuff yesyes
4Vitrophere yesyes
5Tuff yesyes
6Pyroclastic-fall yesyes
7Vitrophere yesyes
8Tuff yesyes
1Not given yesyes
2Not given yesyes
1Rhyolite yesyes
2Rhyolite yesyes
1Basaltic-andesite yesyes
2Basaltic-andesite yes
No NumberRhyolite yesyes