锡矿山矿田狮子山锑矿矿床地质特征及成矿规律

The Geological Characteristics and Metallogenic Regularity of the Shizishan Antimony Deposit in Xikuangshan Orefield

狮子山锑矿位于锡矿山复式背斜北北东倾伏端,与世界锑都锡矿山有相似的成矿条件,具典型的“背斜+一刀”模式,成矿地质条件优越。通过分析研究,验证了该区北东向控矿构造与背斜联合控矿的规律,认为该区近围及深部还有较大的成矿空间,希望能为下一步找矿工作提供一定的帮助。

The Shizishan antimony ore deposit is located at the north-northeast dip end of the Xikuangshan duplex anticline and has similar metallogenic conditions with Xikuangshan,the capital of the antimony world.They all have a typical pattern of"anticline+one slash"and superiorore-forming geological conditions.Through the work in this area,we confirmed that the area has a regularity that the confluence of NE and EW ore-controlling structure controls the mine,thought that there is a large ore-forming space near the periphery and deep part of this area,and hopes to provide some help for the next prospecting work.