Geologic Characteristics of Gold-Bearing Jasperoids and Areas of Possible Additional Occurrences, in the Delta Two-degree Quadrangle, West Central Utah

The Australasian Institute of Mining and Metallurgy
Nutt C. J Campbell D. L
Organization:
The Australasian Institute of Mining and Metallurgy
Pages:
3
File Size:
380 KB
Publication Date:
Jan 1, 1988

Abstract

The Delta two-degree quadrangle is located in west-central Utah, in the eastern Basin and Range physiographic province but near the intersection of the Basin and Range, Rocky Mountain, and Colorado Plateau provinces (Fig. 1). The quadrangle lies in the region of interior drainage that includes western Utah and most of Nevada, and, like the rest of that province, it has an arid climate. This work is part of the United States Geological Survey's ongoing CUSMAP (Conterminous United States Mineral Assessment Program) project in the Delta quadrangle. Trace-element geochemical data presented here includes information from approximately 600 heavy- mineral-concentrate and 2500 rock sample sites from throughout the Delta quadrangle.
Citation

APA: Nutt C. J Campbell D. L  (1988)  Geologic Characteristics of Gold-Bearing Jasperoids and Areas of Possible Additional Occurrences, in the Delta Two-degree Quadrangle, West Central Utah

MLA: Nutt C. J Campbell D. L Geologic Characteristics of Gold-Bearing Jasperoids and Areas of Possible Additional Occurrences, in the Delta Two-degree Quadrangle, West Central Utah. The Australasian Institute of Mining and Metallurgy, 1988.

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