Metamorphic differentiates in the blackbird mining district, Lemhi County, Idaho
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Abstract
Quartz pods and quartz veins devoid of economic minerals occur in the cobalt-copper mineralized Blackbird mining district in Lemhi County, Idaho. These barren quartz bodies are found in regionally and thermally metamorphosed rocks of the Yellowjacket formation (Belt series) of Pre-cambrian age and are believed to be derived from the enclosing quartz-biotite and quartz-biotite-garnet-chloritoid schists by metamorphic differentiation. Other rocks that possibly are products of metamorphic differentiation are discussed. Two zones of regional metamorphism are recognized, a biotite zone and a garnet zone. Contact metamorphism associated with the granitic intrusive rocks of the Idaho batholith is recognized adjacent to the batholith.
Study Area
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Metamorphic differentiates in the blackbird mining district, Lemhi County, Idaho |
Series title | Economic Geology |
DOI | 10.2113/gsecongeo.48.6.447 |
Volume | 48 |
Issue | 6 |
Year Published | 1953 |
Language | English |
Publisher | Society of Economic Geologists |
Description | 10 p. |
First page | 447 |
Last page | 456 |
Country | United States |
State | Idaho |
County | Lemhi County |
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