化工矿产地质Issue(2)：111-114,4.
同位素方法对西八千地下热水的成因分析
ANALYSIS OF THE CAUSE OF THE EIGHT THOUSAND UNDERGROUND HOT WATER BY ISOTOPIC METHOD
宋俊德 1邓怀民 1朱锦程 1王岩 1王宁1
作者信息
摘要
Abstract
Liaoning Linghai Xibaqian geothermal field is located in the western edge of the area of Liaohe basin,and it’s belong to the Cenozoic sedimentary basin geothermal field of heat conduction.To achieve a relatively high temperature of underground water,determine the exploitation of geothermal reservoirs are the sandtone and conglomerate aquifer among third and fourth section of Shahejie Formation of bottom Tertiary.Take a group of geothermal water samples were detected for stable isotopes (18O, 2H,) and radioisotope (14C,3H). HO,3H,14C isotope method are applied to analyze causes of underground water.Showed that underground water is a mixture of the early sedimentary water and recent atmospheric precipitation runoff water together.关键词
同位素/西八千/地下热水/地热资源/成因分析Key words
isotope/Xibaqian/geothermal water/geothermal resources/cause analysis分类
天文与地球科学引用本文复制引用
宋俊德,邓怀民,朱锦程,王岩,王宁..同位素方法对西八千地下热水的成因分析[J].化工矿产地质,2015,(2):111-114,4.
