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The Schwarzwalder uranium deposit, III: alteration, vein mineralization, light stable isotopes, and genesis of the deposit.

Economic Geology

By:
and

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Abstract

The Schwartzwalder uranium deposit was formed during Laramide uplift from groundwaters enriched in ore elements leached from the Proterozoic metavolcanic and metasedimentary host-rocks. Contributions from an unseen intrusive or from Phanerozoic sedimentary rocks are inconsistent with the data. Two stages of alteration and three stages of vein mineralization are related to evolution of CO2, in part episodically.-G.J.N.

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
The Schwarzwalder uranium deposit, III: alteration, vein mineralization, light stable isotopes, and genesis of the deposit.
Series title:
Economic Geology
Volume
81
Issue:
4
Year Published:
1986
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Economic Geology
First page:
872
Last page:
888
Number of Pages:
17