福建省德化邱村金矿床地质特征和找矿方向

Geological Features and Ore-hunting Indicators of Qiucun Gold Deposit in Dehua County,Fujian Province

福建省德化县邱村金矿床主要受构造断裂带控制 ,北东向断裂和近东西向断裂与成矿关系密切。主断裂既为导矿构造 ,也是容矿构造。单矿体定位于其主构造与次一级构造或次级构造与其它构造的交汇部位 ,形成富金矿包。闪长玢岩可作为该区主要的找矿标志。

The Quicun Gold Deposit in Dehun County,Fujian Proince is controlled by the tectonic faulted zones.The north east and east west faults have a close relation with mineralization.The main faults are the orefluid passageways as well as host structures.The simple orebody is located in the intersection parts between the main structures and secondary structures or between the secondary and other structures,which can form a gold ore shoot.The diorite porphyrite has been regarded as an ore hunting indicator in the surveyed area.