渣滓溪锑矿带地质特征及控矿因素与找矿

对渣滓溪锑矿带地质地球化学特征研究表明，矿床赋存于元古代火山—沉积岩系中，赋矿地层具有成矿元素高含量、高离散和双峰态分布特征。成矿严格受断裂构造控制，矿脉成群、成组、带状分布，侧伏延深，属中低温热液充填脉状锑矿床。考虑到湖南锑矿找矿现状，该类型矿床应引起重视。

THE GEOLOGICAL FEATURE AND ORE CONTOR FACTOR OF SITIBUM ORE BELT OF ZHAZIQI, AND ITS GEOLOGICAL PROSPECTION

The geochemical property of Zhaziqi sitibum ore belt demonstrate the sitibum ore deposits occrence in the volcano sedimentaty rock series of proterzoic.It is high on the contents and discrele index of the ore forming element in host formation.Their morphological feature are double peaking on the distributed graph.The mineralization of sitibum was strict controlled by the faulted structure.The minerad diposits of sitibum are a mesothermal low hydrothermal vein diposit.The group of lodes are zoningdistribution,and extend toward leteral pitch. This mineral diposit type merits amportance that think situation on the geological pospection of sitibum in Hunan province.