Hydrothermal alteration in the southeast part of the Frisco quadrangle, Beaver County, Utah / by Bronson Stringham.
A very small amount of pyrite, pyrolusite, and autunite are also found. Late hot spring activity deposited siliceous sinter and native sulphur. Except for perahps the hematite stage, it is believed that the solutions which affected the alteration and minerlaization were strongly acid in nature.
Saved in:
| Main Author: | |
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| Format: | Government Document Book |
| Language: | English |
| Published: |
Salt Lake City :
Utah Geological and Mineralogical Survey affiliated with College of Mines and Mineral Industries, University of Utah,
1963.
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| Series: | Special studies (Utah Geological and Mineralogical Survey) ;
4. |
| Subjects: |
Earth Sciences & Map Library - Stacks
| Call Number: |
TN24.U8 A315 no. 4
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| TN24.U8 A315 no. 4 | Available Place a Hold |