Geology, alteration, and geochemistry of the McGinness Hills area, Lander County, Nevada

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Authors

Wendall, Daniel E.

Issue Date

1985

Type

Thesis

Language

en_US

Keywords

Hydrothermal Systems , Mcginness Hills , Quartz + Kaolinite + Alunite Alteration Of Andesite , Hot-spring Systems , Quartz + Adularia Alteration Of Rhyolite Ash-flow Tuff , Andesite , Porphyry Mo System , Sinter Terraces , Au , Ag , Hg , Sb , Base Metals , Au Enrichment , Ag Enrichment , As Enrichment , Hg Enrichment , Silica Stages , Precious-metal Values , Late Banded Quartz/chalcedony + Adularia Veins , Geochemical Anomalies , Geochemical Alteration , Geochemical Deformation , Co2 , H2s , Mackay Theses and Dissertations Grant Collection

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Abstract

Two distinct hydrothermal systems have been active in McGinness Hills: an older (35 m.y.) system characterized by quartz + kaolinite i alunite alteration of andesite, and a younger (2.7 m.y.) hot-spring system that produced quartz + adularia alteration of rhyolite ash-flow tuff and andesite. The older system is characterized by elevated F and scattered Mo and W anomalies, suggesting that this terrane may overlie a porphyry Mo system. The younger system formed sinter terraces and deposited Au, Ag, Hg, and Sb within 300 feet of the surface with low values of associated base metals. Au enrichment occurs above Ag, As and Hg enrichment; Sb is concentrated within the sinter. Three distinct silica stages are recognized. The highest precious-metal values are associated with late banded quartz/chalcedony + adularia veins. The patterns of geochemical anomalies, alteration, and deformation may be related to the loss of CO2 and H2S from the fluid during boiling.

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Thesis Number: 1976.
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University of Nevada, Reno

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In Copyright(All Rights Reserved)

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