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武宁县石渡锑矿控矿地质因素及成矿机理
引用本文:陈波.武宁县石渡锑矿控矿地质因素及成矿机理[J].江西地质,1999,13(1):50-56.
作者姓名:陈波
作者单位:江西地质矿产勘查开发局赣西北地质大队
摘    要:本语文系统地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 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。

关 键 词:锑矿  控矿构造  成矿机理  石渡  武宁县
修稿时间:1998-12-11

ORE-CONTROLLING GEOLOGICAL FACTORS AND MECHANISM OF FORMATION OF THE SHIDU ANTIMONY DEPOSIT IN WUNING COUNTY
Chen Bo.ORE-CONTROLLING GEOLOGICAL FACTORS AND MECHANISM OF FORMATION OF THE SHIDU ANTIMONY DEPOSIT IN WUNING COUNTY[J].Jiangxi Geology,1999,13(1):50-56.
Authors:Chen Bo
Abstract: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.
Keywords:antimony deposit  ore-controlling    structure  mechanism of ore formation  Shidu      Wuning County
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