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向阳坪铀矿床断裂构造原生晕特征及找矿意义

The Characteristics of Original Geochemical Halo in Fault Zone and Its Prospecting Significance in Xiangyangping Uranium Deposit

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【作者】 欧阳平宁黄满湘刘鑫扬陈跃肖建军

【Author】 OUYANG Ping-ning1,2,HUANG Man-xiang1,LIU Xin-yang3, CHEN Yue2,XIAO Jian-jun2(1.School of Geosciences and Info-physics,Central South University,Changsha,Hunan 410083,China; 2.Research Institute No.230,CNNC,Changsha,Hunan 410013,China; 3.Administration of Geology and Mineral Resource,CNNC,Beijing 100013,China)

【机构】 中南大学地球科学与信息物理学院核工业230研究所中国核工业集团公司地质矿产事业部

【摘要】 向阳坪铀矿床是受断裂构造控制的热液充填型铀矿床,其控矿断裂构造带原生晕轴向分带序列为:Ni-Rb-Bi-Sn-Cu-W-Hg→As-U-Sb-Mo→Sr-Zn,具构造叠加晕特征,反映其成矿具有多期多阶段性;构造原生晕分布特征表现出铀矿化在轴向上具有多个富集带,在走向上亦显示出相同的矿化分布特点,这一特征具有重要的找矿意义。

【Abstract】 Xiangyangping uranium deposit is a hydrothermal filling deposit controlled by faults.The axial zonation of original element along the fault is in sequence of Ni-Rb-Bi-Sn-Cu-W-Hg→As-U-Sb-Mo→Sr-Zn which shows the characteristic of superimposed halos and multiphase mineralization.The distribution characteristic of original halos along structure suggests that uranium mineralization may possess multi-enrichment zones along axial and strata tend.These characteristics are of prospecting significance.

  • 【分类号】P619.14
  • 【被引频次】13
  • 【下载频次】173
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