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应用地球化学方法讨论 开封地热田地下热水的补给来源
引用本文:朱命和,付中,刘彦兵.应用地球化学方法讨论 开封地热田地下热水的补给来源[J].物探与化探,2005,29(6):493-496.
作者姓名:朱命和  付中  刘彦兵
作者单位:河南省地矿局,第十一地质队,河南,商丘,476000
摘    要:应用同位素(D 、18O、14C)地球化学方法, 研究大气降水和地下热水中同位素组成之间成因关系, 分析开封地热田中地热水补给来源方向和地热水的形成, 计算其生成年龄。

关 键 词:热储层  稳定同位素  放射性同位素  
文章编号:1000-8918(2005)06-0493-04
收稿时间:03 22 2004 12:00AM
修稿时间:2004-03-22

A DISCUSSION ON THE SUPPLY SOURCE OF UNDERGROUND HOT WATER IN THE KAIFENG GEOTHERMAL FIELD BASED ON GEOCHEMICAL METHODS
ZHU Ming-he,FU Zhong,LIU Yan-bing.A DISCUSSION ON THE SUPPLY SOURCE OF UNDERGROUND HOT WATER IN THE KAIFENG GEOTHERMAL FIELD BASED ON GEOCHEMICAL METHODS[J].Geophysical and Geochemical Exploration,2005,29(6):493-496.
Authors:ZHU Ming-he  FU Zhong  LIU Yan-bing
Institution:No. 11 Geological Party, Henan Bureau of Geology and Mineral Resources,Shangqiu 476000,China
Abstract:Using isotopic(D,~(18)O,~(14)C)geochemical methods,this paper has studied the genetic relationship between the isotopic composition of meteoric water and that of underground hot water,analyzed the supply source of the Kaifeng geothermal field and the generation of the geothermal water,and calculated its formation age.
Keywords:thermal accumulation layer  stable isotope  radioactive isotope  D
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