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The Copper and Uranium Deposits of the Coyote District, Mora County, New Mexico
From abstract: The copper and uranium-vanadium deposits of the Coyote district, Mora County, N. Mex., are confined to the lower 2,000 feet of the Sangre de Cristo formation of Pennsylvanian and Permian age. A narrow belt of deposits in steeply dipping or overturned rocks extends for 7 miles along Coyote Creek south of Guadalupita. Earlier studies showed that the copper deposits contained uranium, but both the reserves and the uranium content of the copper-bearing shale are too low to permit the recovery of uranium. However, small, commercial grade uranium deposits have been discovered in sandstone.
Date:
December 1954
Creator:
Tschanz, Charles M.; Laub, D. C. & Fuller, G. W.
System:
The UNT Digital Library
The Copper and Uranium Deposits of the Coyote District, Mora County, New Mexico
A report about copper and uranium deposits of the Coyote district, Mora County, N. Mex., are confined to the lower 2,000 feet of the Sangre de Cristo formation of Pennsylvanian and Permian age.
Date:
December 1954
Creator:
Tschanz, C. M.; Laub, D. C. & Fuller, G. W.
System:
The UNT Digital Library