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《Journal of Jilin University(Earth Science Edition)》 2008-S1
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Geological Character and Genesis of Sankuanggou Copper(Iron) Mineral Deposit,Duobaoshan Area,Heilongjiang Province

WANG Hong-yu,MA Li-ling,WANG ZhuoHeilongjiang Institute of Geological Survey,Harbin 150036,China  
Shankuanggou copper(iron) mineral deposit is located in the north-west of the Duobaoshan huge copper(molybdenum) mineral deposit,with the distanced 17 km,it is the model skarn type mineral deposit.This mineral deposit are existed in the grained calcium iron garnet skarn,which are the replaced products of Duobaoshan Formation marble lens it was because of the late-Yenshan-period granodiorite introducing.The mineral deposit was controlled by the north-west(Sankuanggou crossrange anticline) with the north-east(Sankuanggou rift) crossing structure.The ore body were controlled by the north-west sub-fractured structures or the middle-bed structures,the north-east structures were the lead ore body or sub-hold ore body.The genesis of this mineral deposit is the introduced by granodiorite,leading up the skarn of the marble,and replacing by the iron solution,filling or replacing the skarn along the structure fracture or the weak belts by the quartz-sulfide period solution it is contained the copper,forming the copper ore bodies.
【CateGory Index】: P618.41
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