Host rockLimestone · Bolsa Quartzite;Abrigo Limestone
StructureOverthrust Of Bolsa Quartzite Over Paleozoic Rocks. Post Thrust Faults Strike From Ns To Nw-Se And Dip From 50 To 70 Degrees East. They Have Broken The Thrust Plane Into Irregular Steps. Post Thrust Faulting Was Later Than Mineralization
Economic & production
Development statusProducer
First production1913
Last production1929
Identification
Deposit ID10048114
MRDS IDM800134
RegionNA
Data scoreB
Coordinates31.77402, -109.80954
References
ABGMT 187, P. 83WILSON, E.P. GEOLOGY AND ORE DEPOSITS OF THE COURTLAND-GLEESON REGION ARIZONA BUREAU OF MINES BULLETIN 123 P. 43-44, P. 57ABGMT-USBM FILE DATA