Database name: |
World Sediment-Hosted Cu Deposits |
Compilers: |
R. V. Kirkham, J. J. Carriere, A. Rafer, and P. Born |
Release date: |
2015-01-27 |
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Deposit name(s): |
Centennial (Lisbon Valley) |
Political location(s): |
United States; Province or state: Utah |
Deposit clan (type): |
sediment-hosted copper |
Deposit (sub) types: |
continental redbed; oxide and sulphide copper minerals occur throughout the 90 m stratigraphic section of burro canyon and dakota formations |
Geologic province: |
Lisbon Valley |
Commodities: |
Cu |
Geological ages: |
Early Cretaceous - Cretaceous (host rocks) |
Qualified comments: |
(Applies to: miscellaneous comments) oxide and sulphide copper minerals occur throughout the 90 m stratigraphic section of burro canyon and dakota formations; mineralization is structurally and stratigraphically controlled, adjacent to the Lisbon Valley fault |
References: |
Budinski, D. R., 1993 |
Summary Report on the Lisbon Valley Property, San Juan County, Utah |
Company Report, Summo Mineral Corporation, 37 p. |
Mardirosian, C. A., 1974 |
Mining Districts and Mineral Deposits of Utah (2nd Edition) (Exclusive of Oil, Gas and Water) |
Geological Consultant, Scale 1000000 |
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Production data: |
Report period: from 1969 until 1973; 350,000 metric ton ore; Provisional entry?: yesGrade-commodity information: | Cu: 1.25 percent | Reference: Van Eden, J. G., 1978: Stratiform Copper and Zinc Mineralization in the Cretaceous of Angola; Economic Geology, Volume 73, p. 1154 - 1160 Percent weights allocated to deposit: 100.0% |