StructureMajor 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.
AlterationCentrosymmetric Zones Of Potassic, Phyllic, Silicic, And Propylitic Alteration Mineral Assemblages,
Economic & production
Development statusProspect
Identification
Deposit ID10097340
MRDS IDTC00563
RegionSA
Data scoreC
Coordinates-27.33079, -66.83277
References
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 PCIMRI