The ore knob massive sulfide copper deposit, North Carolina: An example of recrystallized ore
Economic Geology
By: A.R. Kinkel Jr.
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Abstract
Massive and disseminated pyrrhotite-chalcopyrite-pyrite ore replaced a fault zone in Precambrian Carolina Gneiss of Keith (1). Closely following sulfide deposition, vein sulfides and silicates in the wall rock were recrystallized under a rising temperature gradient to coarse-grained unoriented aggregates that contain late pyrite porphyroblasts in pyrrhotite. Boudinage, dilation, and flow structures are common.
Study Area
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | The ore knob massive sulfide copper deposit, North Carolina: An example of recrystallized ore |
| Series title | Economic Geology |
| DOI | 10.2113/gsecongeo.57.7.1116 |
| Volume | 57 |
| Issue | 7 |
| Year Published | 1962 |
| Language | English |
| Publisher | Society of Economic Geologists |
| Description | 6 p. |
| First page | 1116 |
| Last page | 1121 |
| Country | United States |
| State | North Carolina |
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