摘要
以宁乡县斋家冲矿区锰矿床为研究对象,通过对宁乡县斋家冲锰矿的区域地质特征、矿区地质特征、矿体地质特征、矿床成因的研究分析,认为宁乡县斋家冲锰矿床原为生物化学沉积,由于区域变质作用和中生代岩浆侵入影响而发生改造,矿床类型应属沉积变质型锰矿床。同时认为该地区成矿地质条件好,具有一定的找矿前景。
The paper takes the manganese deposit in Zhaijiachong mining area of Ningxiang County.Through the analysis and study of the regional geological characteristics,geological characteristics,ore body geological characteristics and genesis of the manganese deposit,it considers Zhaijiachong manganese deposit belongs to biochemical deposit.Since the regional metamorphism and Mesozoic magmatic intrusion,the deposit is changed.Simultaneously,the ore forming and geologic condition is good so that it has certain ore prospecting potential.
作者
张辉
肖谆
万方良
ZHANG Hui;XIAO Zhun;WAN Fangliang(Research Institute of Hunan Provincial Nonferrous Metals Geological Exploration Bureau,Changsha 410015,China)
出处
《矿业工程》
CAS
2018年第5期1-4,共4页
Mining Engineering
关键词
锰矿床
矿石特征
矿床成因
斋家冲
manganese deposit
ore characteristics
ore genesis
Zhaijiachong