StructureHere, A Northwestward-Trending Dike Of Fine-Grained Granite Porphyry, About Eighty Feet Wide Is Cut By A Fault That Strikes Northeast, And Dips Steeply Northwest
AlterationIn Places, The Granite Porphyry Is Silicified And Marked By Copper Stain
Economic & production
Development statusOccurrence
Identification
Deposit ID10027605
MRDS IDM003496
RegionNA
Data scoreC
Coordinates33.38563, -113.48993
References
WILSON, E.D.; 1933; GEOLOGY AND MINERAL DEPOSITS OF SOUTHERN YUMA COUNTY, ARIZONA: ARIZ. B.M. BULLETIN 134, P. 143