Abstract:The carbonates of the Dodguni area of the Chitradurga greenstone belt, Dharwar Craton, India were studied to understand the Archean diagenetic and palaeodepositional conditions using carbon and oxygen isotopes along with whole-rock geochemistry. These carbonates show significant variation in δ 13 C and δ 18 O (À1.73‰ Vienna Peedee Belemnite [VPDB] to À0.45‰ VPDB and δ 18 O vary from À13.51‰ VPDB to À8.46‰ VPDB, respectively). The rare earth element (REE) + Y (rare earth elements and yttrium) of the studied car… Show more
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