| Lat / long: | -27.33079, -66.83277 |
| Primary: | Copper, Gold |
| Operation type: | Unknown |
| Production size: | None |
| Development status: | Prospect |
| Host rock: | Farallon Negro Complex |
| Host type: | Tuff,Andesite |
| Associated type: | Dacite,Andesite |
| Structure: | Major Lineaments With Trends Ranging From N40 To 80w Have Been Reported, Some Of Which Pass Through Other Mineralized Districts When Extended Into Chile, A Strong Nw-Se Structural Control Is Suggested By Orientation Of Dikes, Veins, And Fractures, And By Elongation Directions Of Intrusive Bodies And Alteration Haloes. |
| Alteration processes: | Centrosymmetric Zones Of Potassic, Phyllic, Silicic, And Propylitic Alteration Mineral Assemblages, |
| MRDS | TC00563 |
| DEP | 10097340 |
| Reference | {Deposit:: SUCHOMEL, B.J., 1985, GEOLOGY OF THE BAJO DE AGUA TAPADE BASE AND PRECIOUS METAL PROSPECT, CATAMARCA PROVINCE, ARGENTINA: TUCSON, UNIVERSITY OF ARIZONA MASTERS THESIS, 72 P}{Other Database:: CIMRI} |
| Reporter | Bolm, Karen S. |