Mineral assemblages and distribution of phyllosilicates composition along the main section of the Agua Rica deposit, Catamarca, Argentina. Implications for future mine development

作者：Franchini Marta^*; Impiccini Agnes; Beaufort Daniel; Patrier Patricia; Anderson Corby G; Pons Josefina

来源：Applied Clay Science, 2012, 67-68: 61-71.

DOI：10.1016/j.clay.2012.05.011

• Porphyry Cu-Mo
• High sulfidation epithermal
• Phyllosilicate minerals
• Flotation, metal recovery

Agua Rica (27 degrees 26%26apos;S-66 degrees 16%26apos;O) is a world class Cu (Mo-Au) deposit located in Catamarca, Argentina, in which the porphyry and high sulfidation epithermal stages usually distant 1 km vertically, are located at the same level of erosion. Seventy one samples and 120 phyllosilicates were analyzed from the study section (E-W 6969400 N) to determine distinctive mineralogical zones which differ not only by their hydrothermal history but also by their potential behavior during the ore processing operations via flotation. In the east side of the section, biotite K1.78-1.67 Na0.05-0.02(Al0.42-0.00Mg3.77-3.22Fe1.46-1.00Ti0.90-0.18Mn0.02-0.01) (Si5.42-4.82Al3.18-2.58) (OHF1.90-1.40Cl0.06-0.04)(4) of the early, high temperature potassic alteration (%26gt;550 degrees C to 370 degrees C) is encapsulated in a phyllic halo dominated by illite K1.73-1.08 Na0.10-0.0(Al3.96-3.49Mg0.36-0.03Fe0.25-0.01Ti0.06-0.0) (Si6.53-6.07Al1.93-1.47) (OHF0.54-0.0Cl0.02-0.0)(4) + quartz + pyrite + covellite + molybdenite + rutile. This mineral assemblage formed from fluids with temperatures %26lt;= 350 degrees C that attained high sulfur fugacity. The clasts of the hydrothermal and mineralized breccia bodies located at the center of the section and to the east contain widespread pyrophyllite K0.05-0.0(Al4.07-3.94Fe0.12-0.01)(Si7.92-7.50Al0.50-0.05)(OHF0.15-0.02Cl0.03-0.0)(4) that had replaced illite at temperatures between 360 degrees C and 280 degrees C. Minor amounts of dickite and widespread kaolinite occur in the advanced argillic and phyllic halos, respectively, as late minerals in clots or in veinlets thus, fluids cooled enough (%26lt;270 degrees and %26lt;200 degrees C, respectively) for their formation. The presence of phyllosilicate minerals is a potential cause of loss in recovery of copper and molybdenite during the flotation process. Carefully planned and controlled comprehensive liberation and flotation testing should be undertaken in conjunction with mineralogical analysis to optimize and quantify recoveries, separations, grades and gangue deportment.

• 出版日期2012-10