摘要
以前发现的赋矿层都是碳酸盐岩,而该矿是泥质粉砂岩,此含矿层是目前本县境内新发现的铅锌矿含矿层位。矿床成因属于沉积成岩矿床类型,兼有成岩后期矿床性质。
All of deposits prospected before are carbonate rocks.The deposit is argillaceous siltstoue which is at ore-bearing layer of lead zinc ore prospected newly.Cause of formation is sedimentary diagenetic type combining with deposit characteristics at late period of diagenesis.
出处
《价值工程》
2011年第29期31-32,共2页
Value Engineering
关键词
砂岩型铅锌矿
沉积相
矿床特征
成因
找矿意义
sandstone-type lead-zinc deposits
sedimentary facies
deposit characteristics
cause of formation
prospecting significance