龙王江锑砷金矿带地质地球化学  

GEOLOGY AND GEOCHEMISTRY OF THE LONGWANGJIANG Sb-As-Au ORE ZONE

作　　者：鲍振襄 

机构地区：[1]湘西地勘25队,吉首乾州416007

出　　处：《地质地球化学》1997年第1期1-5,共5页Geology-Geochemistry

摘　　要：龙王江锑砷金矿带位于湘西雪峰弧形构造带中段西南侧，赋存于板溪群浅变质岩系中，主要为与剪切带有关的破碎蚀变岩型金矿。矿床的某些地球化学标志可作为成矿预测和找矿评价的依据。The drigwangjiang Sb-AsAu ore zone is situated on the southwestern side of the middle sector of the Xuefeng arc-shaped tectonic sone in western Hunan Province and occurs in the light metarnornhic rock series of the Banxi Grop. God deposits are predominated by the altered rock-type ones which are closely related to the shear are. Som geochemical features of the dpeits can be used as the grounds for ore prediction and ore exploration.

关 键 词：锑 砷 成矿 地球化学 金矿床 地质学 

分 类 号：P618.510.4[天文地球—矿床学]