Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

National uranium resource evaluation. Raton Quadrangle New Mexico and Colorado. Final report

Technical Report ·
OSTI ID:6732280

Using National Uranium Resource Evaluation criteria, the Raton Quadrangle (New Mexico and Colorado) contains one environment favorable for uranium deposits, the permeable arkosic sandstone members of the Pennsylvanian-Permian Sangre de Cristo Formation for either peneconcordant or roll-type deposits. The favorable parts of the Sangre de Cristo lie mostly in the subsurface in the Raton and Las Vegas Basins in the eastern part of the quadrangle. An area in the Costilla Peak Massif was investigated for uranium by determining geochemical anomalies in stream sediments and spring waters. Further work will be required to determine plutonic environment type. Environments unfavorable for uranium deposits include the Ogallala, Raton, and Vermejo Formations, the Trinidad Sandstone, the Pierre Shale, the Colorado Group, the Dakota Sandstone, the Morrison Formation, the Entrada and Glorieta Sandstones, Mississippian and Pennsylvanian rocks, quartz-pebble conglomerates, pegmatities, and Tertiary granitic stocks.

Research Organization:
New Mexico Bureau of Mines and Mineral Resources, Socorro (USA)
DOE Contract Number:
AC13-76GJ01664
OSTI ID:
6732280
Report Number(s):
GJQ-005(80)
Country of Publication:
United States
Language:
English