摘要
震旦纪是贵州锰矿的成矿时代之一,研究程度低。以处于黔东锰矿成矿区带南部赋存于震旦系下统陡山沱组中的袁家山锰矿为研究对象,对贵州震旦纪锰矿地质特征进行论述,探讨了矿床成因,研究成果可为找矿者在靶区优化、找矿方面提供一定的线索和思路,以期促进贵州锰矿找矿工作的发展。
Sinian is one of the metallogenic ages of manganese deposits in Guizhou,and the research degree is low.Yuanjiashan manganese deposit,which occurs in the lower Doushantuo formation of Sinian system in the south of Guizhou manganese ore metallogenic belt,will be taken as the research object.The geological characteristics of Sinian manganese deposit in Guizhou are discussed,and the genesis of the deposit is discussed.The research results can provide some clues and ideas for the prospector in the target area and prospecting to promote the prospecting of manganese ore in Guizhou.
作者
杨明坤
李向平
YANG Mingkun;LI Xiangping(The 115 Geological Battalion of Geological and Mineral Exploration and Development Bureau,Guizhou Province,Guiyang,Guizhou 551400,China)
出处
《中国锰业》
2019年第4期11-14,共4页
China Manganese Industry
基金
贵州省地质矿产勘查开发局地质科研项目(黔地矿科合[2016]26号)
关键词
震旦纪锰矿
地质特征
矿床成因
Sinian manganese deposit
Geological characteristics
Genesis of the deposit
