摘要
文章通过对佛子冲铅锌矿床成矿物质来源、构造变形和动力成矿特征分析，提出了承压流体参与下断层活动和流体沿构造薄弱带上升、液压扩容致裂的新观点。
On the basis of a comprehensive analysis on the sources of ore-forming
materials, structural deformation, and features of dynamic metallogenesis, the author puts forward
a new point of view that confined fluid participated in the remobilization of lower fault, ascended
along weak structural zone and produced hydrofractures He think that this deposit belongs to
structural dynamic-dominant polygenetic compound deposit
出处
《广西地质》
1999年第1期21-24,32,共5页
Guangxi Geology
关键词
液压致裂
动力成矿
多因复成矿床
铅锌矿床
hydrofracture, dynamic
metallognesis, polygenetic compound deposit
