AlterationAs A Result Of Contact Metamorphic Processes, Magnetite And Some Hematite Have Locally Replaced Certain Calcareous And Dolomite Beds Of 250-Foot Thick Precambrian, Mescal Limestone.
Economic & production
Development statusOccurrence
Identification
Deposit ID10027083
MRDS IDM001963
RegionNA
Data scoreC
Coordinates33.83813, -110.94653
References
HARPER, C.M., 1964, RECONNAISSANCE OF IRON RESOURCES IN ARIZONA: USBM INFORMATION CIRCULAR 8236, P. 26