Geology Of The Prieta Mine, Parral, Chihuahua

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Greenleaf W. Pickard
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
7
File Size:
240 KB
Publication Date:
Jan 1, 1970

Abstract

The Parral mining district is located in the southern part of the state of Chihuahua in north-central Mexico, in the border area of the physiographic provinces of the Mesa Central and the Sierra Madre Occidental, at an average elevation of 1700 meters. This is one of the most highly productive lead-zinc districts of Mexico. The principal operating units are the Prieta, Santa Barbara and San Francisco mines. The Santa Barbara-San Francisco del Oro area is located 25 kilometers to the southwest of the Prieta mine. It has a system of generally narrow veins in fault zones, entirely in the shale series. The Santa Barbara veins follow long, persistent fractures, while the San Francisco del Oro veins are in relatively short fractures. The Veta Colorada structure, located 5 kilometers to the northwest of the Prieta mine, was a major producer of high grade silver ore with low lead-zinc content during the eary 1900's. It follows a major north-south fault zone in andesite and is noteworthy for a number of wide oreshoots of limited vertical extension along its 10 kilometer length. The Palmilla and Esmeralda mines are on the south end of the Veta Colorada structure. Numerous smaller mines are operating in the Parral area. During the last 45 years the Prieta mine has produced approximately 15,000,000 tons of complex sulfide ore, principally from one single vein. Extensive stoping has
Citation

APA: Greenleaf W. Pickard  (1970)  Geology Of The Prieta Mine, Parral, Chihuahua

MLA: Greenleaf W. Pickard Geology Of The Prieta Mine, Parral, Chihuahua. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1970.

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