Open Fracture In Langbeinite, International Minerals And Chemical Corporation's Potash Mine, Eddy County, New Mexico

The American Institute of Mining, Metallurgical, and Petroleum Engineers
James B. Cathcart
Organization:
The American Institute of Mining, Metallurgical, and Petroleum Engineers
Pages:
3
File Size:
153 KB
Publication Date:
Jan 1, 1949

Abstract

The potash mine of the International Minerals and Chemical Corp. is about 18 miles east of Carlsbad, New Mexico, in sec 1 and 12, T 22 S, R 29 E, N.M.P.M. Potash is produced from two zones in the Salado formation of late Permian age. The lower zone, consisting of a mixture of sylvite (KCl) and halite (NaCl), lies at a depth of about 900 ft, and the upper zone, in which the principal potassium mineral is langbeinite (K2S04.2MgS0d), lies at a depth of about 800 ft. Because of the plastic nature of the material, fractures in the Salado formation are extremely rare and have been noted only on the 800 ft level of the International mine. The open fracture described below is almost unique. Only one other open fracture has been noted, and it was on a working face in the same general area as the one described, but was destroyed before the writer had a chance to examine it. According to J. E. Tong, foreman on the 800 level, this fracture was similar to, but smaller than, the one herein described.
Citation

APA: James B. Cathcart  (1949)  Open Fracture In Langbeinite, International Minerals And Chemical Corporation's Potash Mine, Eddy County, New Mexico

MLA: James B. Cathcart Open Fracture In Langbeinite, International Minerals And Chemical Corporation's Potash Mine, Eddy County, New Mexico. The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1949.

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