华南地质与矿产2017，Vol.33Issue(4)：365-371,7.DOI:10.3969/j.issn.1007-3701.2017.04.005
湖南城步县威溪铜钨多金属矿床控矿因素及找矿方向
Geological Properties, Ore Control Factors and Prospecting Orien-tation of Weixi W-Cu Polymetallic Deposit, Chengbu County, Hunan
摘要
Abstract
Weixi W-Cu polymetallic deposit occurs in the second section of Madiyi Formation,Banxi Group.The host rock is the skarn distributed in circle belts.The size of the depoist (W)has reached medium or above.The major type of the ore is W diopside skarn with Cu,Ag,Ga assiciated,and W diopside skarn with Cu,Ag assiciat-ed. This deposit is strictly controlled by the lithology, structure, magma hydrothermal and alteration. There are prospecting potentials of polymetallic in large size in the deep skarn belts at southeast side and hinge zone of Maoerjie anticline.关键词
铜钨多金属矿床/控矿因素/找矿方向/威溪/城步县/湖南Key words
W-Cu polymetallic deposit/ore control factors/prospecting orientation/Weixi/Chengbu County/Hunan分类
地质学引用本文复制引用
刘焕军,赵辉,王晓凌..湖南城步县威溪铜钨多金属矿床控矿因素及找矿方向[J].华南地质与矿产,2017,33(4):365-371,7.基金项目
湖南省探矿权采矿权价款地质勘查项目(编号20150307)资助. （编号20150307）
