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Geology of the Lisbon Valley uranium district, southeastern Utah

Conference · · Field Conf. Guideb. (N.M. Geol. Soc.); (United States)
OSTI ID:5727863
The Lisbon Valley uranium district is located in the east-central part of the Colorado Plateau. The majority of the uranium deposits occur in the Moss Back Member of the Chinle Formation (Triassic); however, minor amounts of ore have been produced from sandstones of the Culter Formation (Permian). In this paper, the geology of these uranium deposits is detailed. (JMT)
Research Organization:
Canyon Resources Corp., Golden, CO
OSTI ID:
5727863
Report Number(s):
CONF-8110216-
Conference Information:
Journal Name: Field Conf. Guideb. (N.M. Geol. Soc.); (United States) Journal Volume: 32
Country of Publication:
United States
Language:
English