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投稿时间:2017-04-19 修订日期:2017-04-20
投稿时间:2017-04-19 修订日期:2017-04-20
中文摘要: 2013年贵州省有色金属和核工业地质勘查局物化探总队在拖枝—挂登地区开展了1∶5万水系沉积物测量,圈出Cu、Pb、Zn多金属矿找矿4片远景区[2]。以喜山期为主的大规模构造运动切穿岩石圈地幔,构造活动的分层折离和滑脱,引起岩石圈部分熔融及软流圈上涌[4、5、7],与本区碎屑岩、碳酸盐岩建造完成一系列变质作用、叠加改造等成矿作用,形成了一系列喷流—沉积型以Cu、Pb、Zn为主的多金属矿床,通过研究区内矿床成因,显示出本区具备寻找大型—超大型多金属矿床的找矿前景。
Abstract:The stream sediment with the proportion of 1:50000 was taken and four Cu, Pb, Zn polymetallic prospecting areas were marked by Geophysical and Geochemical Survey,Non-ferrous Metals and Nuclear Industry Geological Exploration Bureau of Guizhou,in Tuozhi-Guadeng region,2013. Wide-ranging tectonic movements in Himalayan period cut through the lithospheric mantle,the extensive stratify , extensive strike slip, thrusting and extension movement that form the delamination and slippage of lithosphere, which caused partial melting of lithosphere and asthenosphere upwelling, and a serials of metamorphism, superimposition along with clastic rocks and carbonatite formation. finally, formed exhalation-sedimentary deposit primarily of Cu、Pb and Zn, through the study of the deposits in the region, show that the region has the prospecting potential for large-super large polymetallic deposits.
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基金项目:云南拖枝—挂登地区矿产远景调查项目(中国地质调查局西南项目办,编号:资[2013]01-006-039)资助。
作者 | 单位 | |
胡金锋* | 核工业二八0研究所 | 358261032@qq.com |
刘路 | 贵州有色金属和核工业地质勘查局七总队 | |
黄波 | 贵州有色金属和核工业地质勘查局物化探总队 | 379534338@qq.com |
徐伟钧 | 浙江省水文地质工程地质大队 |
引用文本:
胡金锋,刘路,黄波,徐伟钧.拖枝—挂登地区地球化学特征与矿床成因浅析[J].有色金属(矿山部分),2017,69(5):.
HU Jin-feng,LIU Lu,HUANG Bo,XU Weijun.Analysis on the Geochemical Characteristics and Deposit Genesis in TuoZhi-GuaDeng region[J].NONFERROUS METALS(Mining Section),2017,69(5):.
胡金锋,刘路,黄波,徐伟钧.拖枝—挂登地区地球化学特征与矿床成因浅析[J].有色金属(矿山部分),2017,69(5):.
HU Jin-feng,LIU Lu,HUANG Bo,XU Weijun.Analysis on the Geochemical Characteristics and Deposit Genesis in TuoZhi-GuaDeng region[J].NONFERROUS METALS(Mining Section),2017,69(5):.