36Cl Age Study for Deep Geothermal Water of Guanzhong Basin

被引:0
|
作者
Ma Zhi-yuan [1 ]
Dang Shu-sheng [1 ]
Meng Yang [1 ]
机构
[1] Changan Univ, Environm Sci & Engn Sch, Xian, Peoples R China
关键词
Cl-36; dating; sedimentary water; the age of groundwater; Guanzhong Basin; ROCKS;
D O I
暂无
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
There are abundant geothermal water resources in the deep of Guanzhong Basin, whose origin and renewable ability has been the focus of academic circles. Previous research results of the environmental isotope hydrogeochemistry showed that there was small amount residual sedimentary water formed in the geological time in the deep geothermal water of study area, which was directly related to the sustainable development and utilization of geothermal resources. So this paper uses Cl-36 to study the age of deep groundwater. The results of Cl-36 age show that the biggest age of deep groundwater of Guanzhong Basin is 988.69 similar to 1123.98ka. Geothermal water with different tectonic units, different closed condition and different genetic types has different Cl-36 age.
引用
收藏
页码:581 / 584
页数:4
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