The geology of the Copper Basin ore deposits, Lander County, Nevada

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Authors

Tippett, Michael Charles

Issue Date

1967

Type

Thesis

Language

en_US

Keywords

Ore Deposits , Copper Basin , Supergene Enriched Copper Minerals , Arenites , Cambrian Harmony Formation , Hypogene Metallization , Eocene Quartz Monzonites , Host Rocks , Metamorphism , Fissures , Metasomatized Calcareous Shales , Harmony Formation , Oxidation Of Hypogene Chalcoprite-pyrrhotite-pyrite Tactite Zones , Commercial Supergene Copper Deposits , Secondary Ore Controls , Fracture Intersections , Permeable Conduits , Migrating Copper-bearing Solutions , Sediments , Intrusive Rocks , Supergene Enrichment Process , Mackay Theses and Dissertations Grant Collection

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Abstract

The ore deposits at Copper Basin consist principally of supergene enriched copper minerals contained in arenites of the Cambrian Harmony Formation. Hypogene metallization is thought to be coincident with Eocene quartz monzonites which intrude the host rocks, causing widespread metamorphism. Hypogene ore was introduced via NNE and NNW fissures, filled fissures and replaced metasomatized calcareous shales in the upper part of the Harmony Formation. Subsequent oxidation of hypogene chalcopyrite-pyrrhotite-pyrite tactite zones has formed at least three commercial supergene copper deposits. Important secondary ore controls are fracture intersections with favorable beds, creating permeable conduits for migrating copper-bearing solutions. Considerable alteration of the sediments and intrusive rocks attended the supergene enrichment process.

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University of Nevada, Reno

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In Copyright(All Rights Reserved)

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