CAJ | 학술논문

贵州开阳白马洞铀矿是重要的蚀变型铀矿，通过对白马洞清虚洞组黑色蚀变岩及白云岩风化红粘土和寒武系牛蹄塘组黑色页岩的常量元素、微量元素和稀土元素组成的分析研究，发现铀元素含量与 Re、Se、Pb、Cu、As、Sb、Tl、Zn、Ni、Mo、Co、S 含量为正相关关系，铀含量高，则 Re、Se、Pb、Cu、As、Sb、Tl、Zn、Ni、Mo、Co、S 含量也高，其中 As、Co、Mo、Ni、Re、Tl、Zn、S 具有显著的正相关性，而且地表土壤中 Se、V、Mo 等元素的富集是铀矿找矿的主要标志之一。根据白马洞清虚洞组、寒武系牛蹄塘组黑色页岩、灯影组硅化白云岩的稀土元素配分模式分析，硒富集和铀矿化矿源层不仅是牛蹄塘组黑色页岩，可能有更深部的矿源存在。认为硒富集区是铀矿找矿远景区域；古代炼汞矿渣富集铀矿，值得开发利用和治理。
귀주개양백마동유광시중요적식변형유광，통과대백마동청허동조흑색식변암급백운암풍화홍점토화한무계우제당조흑색혈암적상량원소、미량원소화희토원소조성적분석연구，발현유원소함량여 Re、Se、Pb、Cu、As、Sb、Tl、Zn、Ni、Mo、Co、S 함량위정상관관계，유함량고，칙 Re、Se、Pb、Cu、As、Sb、Tl、Zn、Ni、Mo、Co、S 함량야고，기중 As、Co、Mo、Ni、Re、Tl、Zn、S 구유현저적정상관성，이차지표토양중 Se、V、Mo 등원소적부집시유광조광적주요표지지일。근거백마동청허동조、한무계우제당조흑색혈암、등영조규화백운암적희토원소배분모식분석，서부집화유광화광원층불부시우제당조흑색혈암，가능유경심부적광원존재。인위서부집구시유광조광원경구역；고대련홍광사부집유광，치득개발이용화치리。
Baimadong uranium deposit is an important alteration-type uranium deposit.On the basis of the re-search and analysis on major elements,trace elements and REE compositions of Qingxudong Formation black al-tered rock in Baimadong,weathered red clay from dolomite and Cambrian black shale,a positive correlation in concentration was found between uranium and Re,Se,Pb,Cu,As,Sb,Tl,Zn,Ni,Mo,Co,S.The content of Re,Se,Pb,Cu,As,Sb,Tl,Zn,Ni,Mo,Co,S increases with the increasing of uranium content,of which uranium and As,Co,Mo,Ni,Re,Se,Tl,Zn,S show dramatic positive correlation.Se,V,Mo con-centration in soil was considered as one of the main attributes to prospect uranium deposits.According to the analysis of REE distribution pattern among Qingxudong Formation in Baimadong,Cambrian black shale and si-licified dolomite of Dengying Formation,material source of Se concentration and uranium mineralization were not only originated from Niutitang Formation,but also possibly from deeper material source.Therefore,the Se con-centration area is probably the area that uranium deposits are located in.The ancient slag from mercury smelting concentrates uranium,which is also worth exploring and treating.