摘要
铅锌钼矿床的形成受三个因素控制:结构,地层和热源。上部铅锌矿床沿地层发育,发生在石榴和奥陶纪地层之间。较低的钼矿床位于鲁山组与深藏岩体接触带上。通过对铅锌矿床形成规律的分析以及相应的找矿方法和途径,详细介绍了铅锌矿山的分析。
the formation of Pb Zn Mo deposit is controlled by three factors:structure,stratum and heat source.The upper lead-zinc deposits develop along the strata and occur between the pomegranate and Ordovician strata.The lower molybdenum deposits are located in the contact zone between the Lushan Mountain group and the deep rock mass.Through the analysis of the formation regularity of lead-zinc deposits and the corresponding prospecting methods and methods,the analysis of lead-zinc mines is introduced in detail.
作者
曹志军
胡骥
田军委
CAO Zhi-jun;HU Ji;TIAN Jun-wei(Hunan geological and mineral exploration and Development Bureau 408 team,Chenzhou 423000,China;Hunan Hunan Geological Survey Institute,Chenzhou 423000,China)
出处
《世界有色金属》
2018年第9期116-116,118,共2页
World Nonferrous Metals
关键词
铅锌
成矿规律
找矿
lead and zinc
metallogenic regularity
prospecting