摘要
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.
作者
薛超
刘秀
夏雄刚
赵志坚
孙才红
韦俊杰
XUE Chao;LIU Xiu;XIA Xiong-gang;ZHAO Zhi-jian;SUN Cai-hong;WEI Jun-jie(Secend Team Of Hunan Nonferrosus Metals Geologlcal Exploration Bureau,Xiangtan,Hunan,411102, P.R. China)
出处
《南方金属》
CAS
2021年第5期27-29,51,共4页
Southern Metals
关键词
狮子山
锑矿
矿床地质特征
成矿规律
Shizishan
antimony deposit
the geological characteristics
metallogenic regularity