Replacement barite deposit, southern Independence Mountains, Nevada
Journal of Research of the U.S. Geological Survey
By: Keith B. Ketner
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Abstract
Allochthonous Devonian chert, metaquartzite, and greenstone in the Blue Basin quadrangle,, southern Independence Mountains, Nevada, are mineralized with barite forming a deposit of possible commercial grade and size. Textural evidence indicates that the barite was deposited in the host rocks principally by replacement, to a lesser extent by a process involving displacement and expansion of the host-rock material, and to a very minor extent by fracture filling.
Suggested Citation
Ketner, K.B., 1975, Replacement barite deposit, southern Independence Mountains, Nevada: Journal of Research of the U.S. Geological Survey, v. 3, no. 5, p. 547-551.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Replacement barite deposit, southern Independence Mountains, Nevada |
| Series title | Journal of Research of the U.S. Geological Survey |
| Volume | 3 |
| Issue | 5 |
| Year Published | 1975 |
| Language | English |
| Publisher | U.S. Geological Survey |
| Publisher location | Reston, VA |
| Description | 5 p. |
| First page | 547 |
| Last page | 551 |
| Country | United States |
| State | Nevada |
| Other Geospatial | Independence Mountains, Blue Basin quadrangle, Singletree Creek quadrangle |
| Online Only (Y/N) | N |
| Additional Online Files (Y/N) | N |