Uranium, Rare Earth And Iron Mineralization In Pegmatite At The Bemco Mine Prospect, Cranberry Lake, New Jersey

The American Institute of Mining, Metallurgical, and Petroleum Engineers
Andreas H. Vassiliou John H. Puffer
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
17
File Size:
515 KB
Publication Date:
Jan 1, 1985

Abstract

The Bemco mine area is within the Precambrian igneous and metamorphic rock terrain of the New Jersey Highlands province. Rocks In the area include a pyroxene granite, a hornblende granite, a quartz-oligoclase gneiss and a pegmatite and its host rock, a lens of amphibolite which becomes a sulfide-rich pyroxenite near the ore zone. The ore-bearing zone occurs along the hanging wall and foot-wall contact of the pegmatite which was emplaced discordantly into the amphibolite-pyroxenite.
Citation

APA: Andreas H. Vassiliou John H. Puffer  (1985)  Uranium, Rare Earth And Iron Mineralization In Pegmatite At The Bemco Mine Prospect, Cranberry Lake, New Jersey

MLA: Andreas H. Vassiliou John H. Puffer Uranium, Rare Earth And Iron Mineralization In Pegmatite At The Bemco Mine Prospect, Cranberry Lake, New Jersey. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1985.

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