2011•Acta Geologica SichuanRequires access

Ore Material Source and Ore Genesis for the Datongchang Cu Deposit

Zhongfang Yang

Abstract

The Datongchang copper deposit lies in the Huili fault basin and is a typical sandstone type copper deposit and confined to Cretaceous sandstone and conglomerate.The study of major elements,microelements,REE,isotope compositions and detrital minerals indicates that the ore and the wall rock are congenetic and ore material was derived mainly from the host strata including the basalt and granite.

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Key concepts: Geology, Geochemistry, Basalt, Ore genesis, Cretaceous, Conglomerate, Copper ore, Copper