摘要
论述了板溪锑矿的矿脉特征及空间分布规律，并通过对其分析，得出矿床的成矿断裂构造的产生有四个阶段,其中锑矿化主要与第三阶段有关。
The vein characteristics and spatial distribution of Banxi antimony ore-deposit are reported and analysed in this paper, by which 4 phases of occurrence of ore-forming faultswere recognized, and Sb mineralization took place mainly in the 3rd phase.
出处
《大地构造与成矿学》
EI
CAS
CSCD
1998年第S1期78-82,共5页
Geotectonica et Metallogenia
基金
国家自然科学基金!49772152
关键词
成矿构造
矿脉特征
分布规律
板溪锑矿
Ore-forming structutc, vein characteristics, distribution laws, Banxiantimony ore-deposit
