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作 者:刘复兴 LIU Fu-xing(Xitieshan Branch of Western Mining Co.,Ltd.,Haixi 816203,China)
机构地区:[1]西部矿业股份有限公司锡铁山分公司
出 处:《世界有色金属》2019年第21期178-179,共2页World Nonferrous Metals
摘 要:现阶段对于矿区进行地层是研究是十分重要的一个课题,在实际的矿区地层层序分析的内容以矿区实际的侵蚀面或者是矿区的无沉积作用面为主,包含在这个过程中能够与其进行连接关系并且具有因果关系的岩石层面等内容,还会对地层格架内的岩石关系进行详细的研究,以上就是该门学科的主要研究内容。对于矿区进行地层层序研究最早是起源于上世纪80年代,并且是以地震地层学为基础进行发展。对于矿区进行地层层序的分析已经成为了一项热门的课题;且也成为了对矿区地址结构勘探的重要方法,在我国对于矿区的地层层序分析已经陆续展开。笔者将会在本文的论述中,就青海锡铁山铅锌矿区地层层序进行研究与分析,详细的分析结果如下文所示。At present,it is a very important task to study the strata in the mining area.The content of the actual sequence analysis of the strata in the mining area is mainly the actual erosion surface or the non sedimentary action surface of the mining area,including the rock layer which can be connected with the mining area in this process and has causality,and it will also improve the rock relationship in the stratigraphic framework The above is the main research content of this subject.The study of stratigraphic sequence in the mining area originated in the 1980s and developed on the basis of seismic stratigraphy.It has become a hot topic to analyze the stratigraphic sequence of the mining area,and it has also become an important method to explore the address structure of the mining area.In this paper,the author will study and analyze the stratigraphic sequence of Xitieshan lead zinc mine in Qinghai Province,and the detailed analysis results are shown below.
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