锡矿山锑矿床中方解石基本特征及与矿化的关系  

Fundamental Characteristic of Calcite and the Relation Between Mineralization and Calcite in Xikuangshan Antimony Deposit

作　　者：肖亮明 邹利群 李文革 

机构地区：[1]锡矿山闪星锑业有限责任公司,湖南冷水江417500

出　　处：《中国矿山工程》2006年第6期5-7,47,共4页China Mine Engineering

摘　　要：对锡矿山锑矿床中不同类型的方解石进行了矿物学、地球化学研究,并探讨了方解石形成的物理化学条件与成矿的关系,揭示了方解石与辉锑矿、石英共生的必然性,认为方解石形成与矿化之间有着重要的联系,并指出了如何运用方解石这一重要的找矿标志进行找矿勘探。This paper analyzed diverse calcite in terms of mineralogical and geochemical research, and discussed the relation generating calcite condition and mineralization geneses. It＇s inevitable that calcite, stibnite and quartz are accrete has been revealed. The significant relation between calcite-forming and ore-forming has been given. How to apply the prospecting indication for prospecting ore deposit has been put up.

关 键 词：方解石 矿物学特征 地球化学特征 矿化 

分 类 号：P612[天文地球—矿床学]