摘要
本文系统介绍了武宁县石渡锑矿的基本地质特征，并结合大量的实际地质资料，对矿床的控矿地质因素进行了探讨，认为石渡锑矿不但受区域成矿环境和地层层位及岩石建造的控制，同时控矿构造对矿体空间分布及其形态产状也起重要控制作用。叙述了构造演化与成矿的关系，阐明了控矿构造形式及控矿构造类型。最后对锑矿的成矿机理进行了探讨。
This paper deals systematically with the basic geological features of the
Shidu antimony deposit of Wuning County, highlighting the ore-controlling geological factors on
the basis of a wealth of factual geological data. The author holds that this deposit is controlled
by regional metallogenic environment, stratigraphy and rock formation, although structre plays
a vital role in controlling the spatial distribution, geometry and mode of occurrence of the ore
bodies. This paper has brought out the relation between structural evolution and mineralization,
cast Iights on ore-controlling structural forms and structural types, and finally discussed on the
mechanism of formation of antimony ores.
出处
《江西地质》
1999年第1期50-56,共7页
Jiangxi Geology
关键词
锑矿床
控放地质因素
成矿机理
antimony deposit ore-controlling
structure mechanism of ore formation Shidu Wuning County
