Replacement barite deposit, southern Independence Mountains, Nevada
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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.
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 |
Google Analytic Metrics | Metrics page |