Uranium Dividends From Bacterial Leaching

The American Institute of Mining, Metallurgical, and Petroleum Engineers
R. A. MacGregor
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
2
File Size:
168 KB
Publication Date:
Jan 3, 1969

Abstract

The Stanrock mine of Stanrock Uranium Mines Ltd. is located on Quirke Lake in the Elliot Lake area of northern Ontario, about 25 miles north of Lake Huron. The property was developed and brought into production at a rate of 3000 tons of ore per day during the uranium boom of the mid-1950's. The mine workings are from 1200 to 2100 ft below sea level. Mining was done by the room-and-pillar method with 65 to 80% extraction. The plant is located at an elevation of 1400 ft above sea level. The orebodies are conglomeratic beds, 6 to 40 ft in thickness and dipping 5º to 40º. The ore is a quartz pebble conglomerate with a pyritized sericitic matrix. The ore minerals are brannerite, frequently intergrown with anatase or rutile, uraninite, and some monazite and minor coffinite and thucolite. Sulfides constitute 5 to 10% of the ore as pyrite with minor amounts of pyrrhotite, chalcopyrite and galena.
Citation

APA: R. A. MacGregor  (1969)  Uranium Dividends From Bacterial Leaching

MLA: R. A. MacGregor Uranium Dividends From Bacterial Leaching. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1969.

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