Geology and geochemistry of the Deer Trail Pb-Zn-Ag-Cu manto deposits, Marysvale District, west-central Utah
Economic Geology
By: D.W. Beaty, C. G. Cunningham, R.O. Rye, T. A. Steven, and E. Gonzalez- Urien
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Abstract
Strata-bound sulphide replacement bodies in the Deer Trail mine are sinuous pipes in carbonate beds, approximately localized by an anticlinal axis, and radiate from a fault across the lower part of the Permian Toroweap formation. Indistinct sericitic envelopes provide a K/Ar age of 14 m.y., correlative with barren, altered volcanic rocks above a hypothesized intrusion, 1 km to the west. Lead and sulphur isotope data imply an igneous source. Inclusion data and deuterium and oxygen isotopes imply a magmatic fluid progressively diluted with meteoric waters. The deposits are the outer zone of a volcanic hydrothermal system. -G.J.N.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Geology and geochemistry of the Deer Trail Pb-Zn-Ag-Cu manto deposits, Marysvale District, west-central Utah |
| Series title | Economic Geology |
| DOI | 10.2113/gsecongeo.81.8.1932 |
| Volume | 81 |
| Issue | 8 |
| Year Published | 1986 |
| Language | English |
| Publisher | Geological Society of America |
| Description | 21 p. |
| First page | 1932 |
| Last page | 1952 |
| Country | United States |
| State | Utah |
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