Localization of Pyrometasomatic Ore Deposits At Johnson Camp, Arizona
- Organization:
- The American Institute of Mining, Metallurgical, and Petroleum Engineers
- Pages:
- 6
- File Size:
- 552 KB
- Publication Date:
- Jan 12, 1953
Abstract
The orebodies are long bedding-plane lenses of chalcopyrite and sphalerite, associated with garnetite masses. Most of the orebodies are within a 50-ft thickness of Cambrian limestone; other Paleozoic limestones and dolomites are locally metamorphosed but only slightly mineralized. Pre-mineral faults are numerous, but shallow folds were the main ore-localizing structures.
Citation
APA: (1953) Localization of Pyrometasomatic Ore Deposits At Johnson Camp, Arizona
MLA: Localization of Pyrometasomatic Ore Deposits At Johnson Camp, Arizona. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1953.