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佛子冲铅锌矿田火山岩覆盖区接触-断裂带控矿特征
引用本文:梁锦叶,冯佐海,雷良奇,肖龙,黄亮. 佛子冲铅锌矿田火山岩覆盖区接触-断裂带控矿特征[J]. 桂林工学院学报, 2000, 20(2): 128-131
作者姓名:梁锦叶  冯佐海  雷良奇  肖龙  黄亮
作者单位:1. 南宁有色金属工业学校,广西南宁,530001
2. 桂林工学院,广西桂林,541004
3. 广西地质勘查局204队,广西钟山县,542602
基金项目:广西自然科学基金,中国有色金属工业总公司资助项目,桂科自:9912011,96-D-31,,
摘    要:佛子冲矿田火山岩覆盖区3种地质体间接触-断裂带的矿化特征显示,矿(化)体主要产于正接触带,其次产于外接触带内;Pb,Zn,Cu等主要成矿元素矿化富集强度一般随断层岩的变形程度增大而增高,两者呈明显的正相关关系.

关 键 词:接触-断裂带 控矿特征 铅锌矿田 火山岩覆盖区
修稿时间:1999-08-11

THE ORE CONTROL FEATHER OF CONTACT-FRACTURED ZONE IN THE VOLCANITE-COVERED AREA, FUZICHONG Pb-Zn ORE FIELD, GUANGXI
Liang Jinyie,Fang Zuohai,Lei Liangqi,Xiao Long,Huang Liang. THE ORE CONTROL FEATHER OF CONTACT-FRACTURED ZONE IN THE VOLCANITE-COVERED AREA, FUZICHONG Pb-Zn ORE FIELD, GUANGXI[J]. Journal of Guilin University of Technology, 2000, 20(2): 128-131
Authors:Liang Jinyie  Fang Zuohai  Lei Liangqi  Xiao Long  Huang Liang
Abstract:The mineralization characteristics of contact-fractured zone among the three types of geologic bodies in the volcanite-covered area of Fuzichong ore field show that the mineralizations are mostly located in the right contact zone, and some of them occur in the outside contact zone, the main mineralization elements,such as Pb,Zu,Cu, increase generally with the deformation degree of fault rocks, there is a consistance relation between the mineralization elements and the deformation degree.
Keywords:Pb-Zn deposits  contact-fractured zone  control feather  Guangxi  Fuzichong
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