Abstract
Carbon and oxygen isotopic compositions of carbonates from auriferous quartz carbonate veins (QCVs) of two orogenic gold deposits – Ajjanahalli and Guddadarangavvana Halli (G.R. Halli) – from the Neoarchean Chitradurga schist belt of the Dharwar craton, southern India are examined to understand the origin of the mineralizing fluids. The average carbonate carbon (δ13Cpdb) and oxygen (δ18Osmow) isotope compositions of QCVs of Ajjanahalli are −5.5±1.3‰ and 14.1±2.7‰, respectively. The same ratios for the QCVs of G.R. Halli are −6.2±1.9‰ and 14.1±0.5‰. The corresponding average fluid δ13C and δ18O compositions are −5.81±1.14‰, 13.78±5.1‰ for Ajjanahalli and −4.64±0.7‰, −6.50±0.6‰ for G.R. Halli. The δ13Cpdb of syn-sedimentary carbonates of BIF of Ajjanahalli (−1.8±0.1‰), carbonated metabasalts of Ajjanahalli (−1.4‰) and G.R. Halli (−1.3‰) fall in the compositional range of marine carbonates (0±2‰). As dissolution/decarbonation reactions during metamorphism of pre-existing carbonate/carbonated rocks produce CO2 with δ13C values similar to or more enriched than parent rock, the carbonate or fluid δ13C ratios of the QCVs (which fall in the compositional range of mantle/magmatic derived CO2 or carbonates) obtained in this work cannot be the result of metamorphism. It is proposed that gold mineralizing fluids were derived from juvenile magmatic melts and were channeled through crustal scale shear zones to give rise to the gold deposits.
Published Version
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call