摘要
江南沟锰矿产于寒武纪牛蹄塘组,矿体严格受地层层位和岩性控制,矿床类型为海相沉积型锰矿。鄂西地区寒武纪牛蹄塘组分布广泛,该锰矿可为进一步拓展锰矿勘查层位提供借鉴。
The Jiangnangou manganese ore is produced in the Niutitang Formation.The ore body is strictly controlled by stratigraphic horizon and lithology and the deposit type is marine sedimentary manganese ore.The formation of Cambrian Niutitang Formation in western Hubei is widely distributed,which can be used for reference for further exploration of manganese ore.
作者
黄景孟
张笑
韩杰
赵生贵
孙腾
魏四华
周豹
汪国虎
HUANG Jingmeng;ZHANG Xiao;HAN Jie;ZHAO Shenggui;SUN Teng;WEI Sihua;ZHOU Bao;WANG Guohu(Hubei Geological Survey,Wuhan,Hubei430034)
出处
《资源环境与工程》
2017年第6期696-699,共4页
Resources Environment & Engineering
基金
中国地质调查局湘西-鄂西成矿带地质矿产调查项目的子项目湖北房县西蒿坪地区矿产地质调查(项目编码:12120113062500)
关键词
锰矿
牛蹄塘组
沉积型
地质特征
manganese ore
Niutitang Formation
sedimentary
geological characteristics
