Geohydrology of the Rainy Creek igneous complex near Libby, Montana

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Authors

Zinner, Ronald Eric

Issue Date

1983

Type

Thesis

Language

en_US

Keywords

Rainy Creek , Alkaline-ultramafic Complex , Ultramafic Pluton , Magnetite Pyroxneite , Vermiculite Pyroxenite , Biotite Pyroxenite , Geohydrology , Rainy Creek Igneous Complex , Libby, Montana , Ground-water , Mackay Theses and Dissertations Grant Collection

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Abstract

The Rainy Creek alkaline-ultramafic complex consists mainly of an ultramafic pluton crudely circular in plain view, composed primarily of magnetite pyroxenite, "vermiculite" pyroxenite, and biotite pyroxenite arranged in an inward succession. Weathering of the biotite pyroxenite by groundwaters is concluded to be the major altering process but dilute hydrothermal fluids may have been responsible for a small amount of alteration.

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Thesis Number: 1795.
Online access for this thesis was created in part with support from the Institute of Museum and Library Services (IMLS) administered by the Nevada State Library, Archives and Public Records through the Library Services and Technology Act (LSTA). To obtain a high quality image or document please contact the DeLaMare Library at https://unr.libanswers.com/ or call: 775-784-6945.

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University of Nevada, Reno

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In Copyright(All Rights Reserved)

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