GEOLOGY AND GEOCHEMISTRY OF THE MAMMOTH BRECCIA PIPE, COPPER CREEK MINING DISTRICT, SOUTHEASTERN ARIZONA
The unexposed Mammoth Breccia Pipe was discovered by drilling and has a vertical extent of 915 m and a maximum width of 180 m. The breccia pipe consists of angular clasts of granodiorite cemented by quartz, chalcopyrite, bornite, anhydrite, and calcite. New 40Ar/39Ar geochronology from two biotite samples suggest a minimum age of 62.1 60.8 Ma for the Copper Creek Granodiorite, which was previously dated at 69.7 ± 2.7 and 65.8 ± 1.6 Ma by K-Ar techniques. New 40Ar/39Ar geochronology on six separates of hydrothermal white mica yields an age of 60.0 ± 0.9 Ma., which is interpreted to be the age of associated copper mineralization. Previously, other copper mineralization within the district had been dated at 56.9 ± 0.9 Ma by Re-Os techniques, indicating at least 4 5 m.y. of ore formation.
Fluid inclusion studies suggest that boiling, or unmixing, occurred during copper mineralization. A parent fluid with a salinity of ~ 10 wt. % NaCl equiv. unmixed into a dilute aqueous vapor (1 2.8 wt. % NaCl equiv.) and a hypersaline brine (33.4 35.1 wt. % NaCl equiv.). Final homogenization temperatures of the brine-bearing inclusions were as great as 375°C.
Sulfur isotope geothermometry of two cogenetic hydrothermal phases, anhydrite and chalcopyrite, gives a temperature of mineralization of 469 ± 25°C. Calculated oxygen and hydrogen isotope values for fluids in equilibrium with quartz and white mica range from 10.2 to 13.4 and -60 to -39, respectively, suggesting a dominantly magmatic component within the hydrothermal fluids responsible for mineralization.