Trace metals in pyrite and marcasite from the Agua Rica porphyry-high sulfidation epithermal deposit, Catamarca, Argentina: Textural features and metal zoning at the porphyry to epithermal transition

Abstract

Agua Rica is a world-class Cu (Mo–Au) deposit located in Catamarca, Argentina, in which the porphyry and high sulfidation epithermal stages are juxtaposed due to the telescoping of the mineralizing system. Pyrite is the most abundant sulfide in the analyzed section of the deposit and shows variations in textures and tracemetal content (determined by LA–ICPMS), between the porphyry and epithermal stages. Pyrite from the porphyry stage is fine grained and depleted in most trace elements analyzed, except for traces of Co (up to 276 ppm) and Ni (up to 131 ppm). Pyrite from the epithermal stage is texturally complex, compositionally heterogeneous, and the trace metal content varies with depth and within sub-stages of mineralization. At an intermediate depth (2625 m), epithermal pyrite from the cement of the jig-saw and clast-supported hydrothermal breccias are enriched in Cu (up to 2961 ppm) that correlates with the highest Cu grades in the section. This pyrite contains micro-inclusions of sulfosalt minerals as inferred by LA–ICPMS elemental mapping and individual spot ablation profiles. They are zoned and show a Co-rich core, an intermediate zone enriched inCu, and anouter rimrich inZn.At shallower levels (3000m), epithermal pyrite cements in the heterolithic hydrothermal breccia are unusually rich in trace metals that correlate with the highest Pb, Zn, Au, and Ag grades. The ore-stage pyrite occurs as either successive colloform bands on earlier Co-bearing cores or as veinlets infill. The colloform pyrite bands and veinlets are As-poor (b30 ppm) and enriched in Pb (up to 4528 ppm), Cu (up to 3900 ppm), Zn (up to 1078 ppm), Ag (up to 136 ppm), Au (up to 6.7 ppm), Bi (up to 1077 ppm), and Te (up to 3.1 ppm). In LA–ICPMS elemental maps, arsenic concentrates in a thin inner band within the thicker, trace element-rich rims. The colloform banding in pyrite is interpreted to reflect rapid crystallization during fluid boiling at a hydrothermal fluid–meteoric water interface, creating intense fluctuations in temperature and producing undercooling in the mixed fluid. This late and shallow fluid was depleted in As and Cu and also precipitated alunite, Fe-poor sphalerite, and marcasite enriched in trace metals. Maximum Au and Ag inputs into the system occurred towards the end of the epithermal cycle and are expressed by the Au–Ag-rich rims in hydrothermal pyrite. Based on Au–As data in pyrite, ore fluids forming early pyrite were undersaturated with respect to native Au (solid solution incorporation), while later fluids precipitating colloform pyritewere supersaturated with respect to native Au forming Au nanoparticles. This study provides evidence that pyrite records chemical changes at the porphyry to epithermal transition that can be used tomonitor hydrothermal fluid evolution, constrain different mineralization stages, and vector towards undiscovered ore zones.