Ore controlThe Main Porphyry Dikes Strike Approximately Parrallel To The Limestone, But Branches Of Them Trend Northeast, And South. In General The Dikes Dip Steeply Northward, But In Places They Form Sills More Or Less Concordant With The Limestone Beds.
Materials
Ore mineralsAnglesite, Hemimorphite, Smithsonite
GangueGarnet
Geology
Host rockLimestone
Associated rockPlutonic Rock
Structure1200 Feet Of The Shaft Is The O'Carrol Fault.
Economic & production
Development statusPast Producer
Identification
Deposit ID10026851
MRDS IDM000507
RegionNA
Data scoreC
Coordinates33.06148, -110.77708
References
WILSON, E. D., 1951 , ARIZONA ZINC AND LEAD DEPOSITS: ARIZONA BUREAU OF MINES, BULLETIN 158ARIZONA BUREAU OF MINES BULLETIN NO. 158 .