全安盆地水文地质特征及热水成因分析
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  • 英文篇名:The Characteristics of Hydrogeological and Analysis of Genesis of Geothermal Water in Quan'an Basin
  • 作者:唐仕尧 ; 江卫兵 ; 王联社
  • 英文作者:TANG Shi-yao;JIANG Wei-bing;WANG Lian-she;No.290 Institute,CNNC;
  • 关键词:地下热水 ; 氢氧稳定同位素 ; 成因分析 ; 循环条件 ; 全安盆地
  • 英文关键词:geothermal water;;stable H-O isotope;;characteristics and source of geothermal water;;groundwater cycling conditions;;Quan'an basin
  • 中文刊名:HDDZ
  • 英文刊名:Journal of East China Institute of Technology(Natural Science)
  • 机构:核工业二九0研究所;
  • 出版日期:2014-09-30
  • 出版单位:东华理工大学学报(自然科学版)
  • 年:2014
  • 期:v.37;No.127
  • 基金:中国地质调查局“全国铀矿资源调查”项目(1212011220781);; 国家科技支撑计划项目(2011BAB04B07);; 中国核工业地质局生产中科研项目(201369)
  • 语种:中文;
  • 页:HDDZ201403016
  • 页数:6
  • CN:03
  • ISSN:36-1300/N
  • 分类号:89-94
摘要
在简要分析全安盆地水文地质特征、地下水赋存条件及划分地下水类型基础上,对盆地西部周地—暖水塘地区地下热水形成原因、赋存环境进行研究,认为多期次构造运动形成的断裂、裂隙沟通深部地下热水是盆地热水来源的主要原因;采取地下热水样品并开展氢氧稳定同位素、逸出气体、水化学成份测试,认为地下热水由大气降水补给,长期水动态观测结果也显示大气降水与地下热水关系较密切。
        Based on the analysis of hydrogeological characteristics,groundwater storage conditions and division of groundwater types,this research analyze the cause and conditions of geothermal water in Zhoudi-Nuanshuitang area in the western of Quan'an basin. The result shows that the connectivity between upper and bottom layers of geothermal water by the faults caused by poly-period secondary tectonic movement was the main source for current geothermal water. Then,the groundwater was sampled and analyzed by stable H-O isotope technique,escaping gas detection and water chemical composition test,the results indicate that water form atmospheric precipitation was the supply source of the geothermal water. These results also can support by a long-term water dynamic observation,which believe that a close relationship between geothermal water and precipitation.
引文
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    1王联社,江卫兵,唐仕尧,等.2010.广东省南雄市坪下水地区铀矿普查报告[R].核工业二九〇研究所报告.
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