摘要
根据化学分析和同位素测定结果,广东地下热水主要是大气降水起源,水中F^-、HCO_3^-、气体组分是映震较灵敏的组分,这与其特定的地球化学背景条件有关。
On the basis of chemical analyses and fsotopic measurements, the source of Guangdong underground hot-water is mainly atmospheric precipitation. The gaseous composition of gas F-. HCGs' in water are sensitive to seismic actively which is related with the specific condition of underground chemical background.
出处
《地震》
CSCD
北大核心
1993年第3期64-67,共4页
Earthquake
基金
地震科学联合基金
