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甘肃省花海盆地土壤氡分布特征及控制因素研究

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文章导航 > 西北地质 > 2020 > 53(3): 106-112

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雷波, 贺锋, 陈冠, 刘伟, 鲁宝龙. 2020. 甘肃省花海盆地土壤氡分布特征及控制因素研究. 西北地质, 53(3): 106-112. doi: 10.19751/j.cnki.61-1149/p.2020.03.009
引用本文: 雷波, 贺锋, 陈冠, 刘伟, 鲁宝龙. 2020. 甘肃省花海盆地土壤氡分布特征及控制因素研究. 西北地质, 53(3): 106-112. doi: 10.19751/j.cnki.61-1149/p.2020.03.009
shu
LEI Bo, HE Feng, CHEN Guan, LIU Wei, LU Baolong. 2020. Radon Distribution Characteristics and Controlling Factors in the Soil of Huahai Basin, Gansu Province. Northwestern Geology, 53(3): 106-112. doi: 10.19751/j.cnki.61-1149/p.2020.03.009
Citation: LEI Bo, HE Feng, CHEN Guan, LIU Wei, LU Baolong. 2020. Radon Distribution Characteristics and Controlling Factors in the Soil of Huahai Basin, Gansu Province. Northwestern Geology, 53(3): 106-112. doi: 10.19751/j.cnki.61-1149/p.2020.03.009
shu

甘肃省花海盆地土壤氡分布特征及控制因素研究

  • 1. 南华大学资源环境与安全工程学院, 湖南 衡阳 421001;

  • 2. 核工业北京地质研究院, 北京 100029;

  • 3. 核工业二0三研究所, 陕西 咸阳 712000

  • 基金项目:

    湖南省自然科学基金（2019JJ50525），湖南省教育厅科技项目（180SJK022），衡阳市科技指导性项目（S2018G9031015322），中国核工业地质局项目（No.201827-02）

详细信息
    作者简介: 雷波(1985-),男,讲师,博士,主要从事氡测量和地质勘查与研究工作。E-mail:hame88@126.com

  • 中图分类号: P595

Radon Distribution Characteristics and Controlling Factors in the Soil of Huahai Basin, Gansu Province

  • 1. School of Resource&Environmental and Safety Engineering, University of South China, Hengyang 421001, Hunan, China;

  • 2. Beijing Research Institute of Uranium Geology, Beijing 100029, China;

  • 3. No. 203 Research Institute of Nuclear Industry, Xianyang 712000, Shaanxi, China

    摘要
  • 花海盆地位于甘肃省走廊盆地群西缘，是中国深部铀资源勘探的重要潜力区之一。根据对土壤氡气浓度信息提取和野外勘探钻探成果分析，花海盆地土壤氡浓度可分为东部正常场-偏高场氡晕和西部偏高-高场晕氡晕；下白垩统下沟组（K1x）砂岩层段为本区铀矿化有利层位，建议在西部、南部土壤氡气偏高-高场晕氡晕过渡带追索层铀矿化带，寻找有利靶区。
    Huahai basin is located in the western margin of Corridor basins in Gansu Province, and is one of the important potential areas for deep uranium exploration. Based on the extraction of radon gas in soil and the information of the field exploration, it is considered that the soil radon concentration in Huahai basin can be divided into normal to high in the east and even higher in the west. The Lower Cretaceous sandstone of Xiagou Formation (K1x) is the target reservior of uranium deposits in the study area. The authors suggest that the favorable target is in the transition zones and uranium mineralization belt with higher Radon levels in the west and south of the area.
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收稿日期:  2020-01-13
修回日期:  2020-06-02

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