Replacement barite deposit, southern Independence Mountains, Nevada

Keith B. Ketner

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USGS · 70156574

Replacement barite deposit, southern Independence Mountains, Nevada

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.

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Journal of Research of the U.S. Geological Survey Article

Source-reported bounding extent: 40.78470081841747° to 41.934976500546604° latitude; -116.57318115234375° to -115.72723388671875° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Keith B. Ketner. 1975. Replacement barite deposit, southern Independence Mountains, Nevada. https://pubs.usgs.gov/publication/70156574

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