The metallogenic mechanism of the sandstone-type copper deposits in the Chuxiong Basin, Yunnan Province

The sandstone-type Cu deposits in the Chuxiong Basin occur in the Cretaceou s Gaofengsi Formation and the Maotoushan Formation and the orebodies are st ratoid and lenticular in term, structurally controlled by their stratigraph ical position. Ore structures are dominated by impregnated and striped ones . In addition, it has been observed that copper mineralization is controlle d by water-discharge and deformation structures, Orebodies are commonly see n on the gently inclined limbs of the anticline, with the involution front. Copper mineralization shows a distinct zonation. S, Pb isotope and REE dat a suggest that the copper would stem from the country rocks and the sulfur largely from the lower strata, During diagenesis oxidized Cu-bearing brines derived from the upper parts and reduced brines from the lower parts are i nvolved in metallogenetic reactions in the stress neutral plane, which is t he key to the formation of copper deposits in the Chuxiong Basin.