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鄂东南某铀矿勘查区地气与X荧光异常特征及找矿意义
引用本文:张国亚,周四春,刘晓辉,刘俊,杨奎,朱剑.鄂东南某铀矿勘查区地气与X荧光异常特征及找矿意义[J].高校地质学报,2014,20(4):564.
作者姓名:张国亚  周四春  刘晓辉  刘俊  杨奎  朱剑
作者单位:成都理工大学核技术与自动化工程学院,成都,610059
基金项目:国家自然科学基金项目(41074094);四川省教育厅重点科技项目(10ZA118);成都理工大学“核安全工程优秀创新团队”
摘    要:采用地气与土壤X荧光(地球化学) 测量法,对鄂东南某铀矿勘查区开展隐伏铀矿找矿工作,结果表明铀矿赋存在
工作区主断裂和次级断裂中,在含矿断裂上方及断裂延伸方向的相邻区域形成含U的地气与土壤地球化学异常区。异常区
内Pb,Zn,Cu,Au的地气异常明显且具有一定的差异,同时伴有幅度较低的W,Bi,Y,Mo,Mn,As等元素组合异常。
根据勘查区获得的地气与土壤X荧光资料综合分析,在测区西北的次级断裂F7北部捕获的地气与土壤异常具有已知矿异常
的全部特征。依据地气异常位置与断裂的关系,推断铀矿可能埋深在200~350 m左右,矿体在走向上可能有220 m的延续。目
前,在该异常区布设的钻孔已在200 m深度见到铀矿体,进一步的探矿工程还在进行中。

关 键 词:地气测量  土壤X荧光测量  异常特征  隐伏铀矿  找矿预测

The Abnormal Features and Prospecting Significance of Geogas and X-ray Fluorescence in Exploration Area of Uranium Deposits in Southeastern Hubei Province
ZHANG Guoya,ZHOU Sichun,LIU Xiaohui,LIU Jun,YANG Kui,ZHU Jian.The Abnormal Features and Prospecting Significance of Geogas and X-ray Fluorescence in Exploration Area of Uranium Deposits in Southeastern Hubei Province[J].Geological Journal of China Universities,2014,20(4):564.
Authors:ZHANG Guoya  ZHOU Sichun  LIU Xiaohui  LIU Jun  YANG Kui  ZHU Jian
Abstract:We have carried out concealed uranium ore prospecting by geogas and soil X-ray fluorescence (geochemistry) measurements in the exploration area of uranium deposits in southeastern Hubei Province. Measurements of the known uranium mining areas show that uranium occurs in the primary and secondary fractures. Above the ore fractures and along the direction extended from the fracture in the adjacent area, forms the geogas and soil geochemical anomaly area of uranium. In the abnormal zone, Pb, Zn, Cu, Au in the geogas show anomalies, but also show obvious difference. The anomalies are accompanied by low amplitude anomalies in W, Bi, Y, Mo, Mn, As and so on. According to the comprehensive analyses of exploration area with geogas and soil X-ray fluorescence data, the northwest part of the surveyed area north of the secondary fracture F7 captured all the characteristics of geogas and soil with known ore anomaly. According to the relationship between abnormal position of geogas and fracture, uranium may be buried at the depth of 200~350 m, on to the ore body, extending 220 m along the strike. At present, uranium ore bodies have been confirmed in the abnormal area in a borehole at 200 m depth. Further exploration engineering work is in progress.
Keywords:geogas survey  X-ray fluorescence measurements of soil  abnormal features  concealed uranium  ore-prospecting
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