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《Geology and Prospecting》 2008-01
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DISTRIBUTION CHARACTER OF SULFUR ISOTOPE IN THE DUOBAOSHAN COPPER DEPOSIT

FENG Jian-xing(No.5 Institute for Geological Exploration of Heilongjiang Province,Heihe 164300)  
Duobaoshan Cu deposit is a big porphyry copper deposit,which is located in the bound of Daxin'anling uplift zone and Songliao subsidence zone.Outcrop strata are mainly middle Ordovician Duobaoshan formation.Intrusive rocks mainly include granodiorite porphyry and granodiorite in the late period of Variscan movement.Around granodiorite porphyry there exists wallrock alteration zonation,showing potassium alteration,sericitization and propvlitization zonation from inner to outside.Ore bodies are most located in sericitization zone.It is shown that Duobaoshan Cu deposit was formed in a low temperature,in which metal sulfides have zonation as bornite,chalcopyrite and pyrite from the center to the edge.Based on sulfur isotope distribution character and homologous relationship with bonanza in Duobaoshan Cu deposit,some forming characters are analyzed.
【CateGory Index】: P618.41
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