摘要
本文阐述了五大连池矿水形成的地质条件,矿水中CO_2气体形成过程及其演化趋势。根据^(13)C、^(18)O等同位素测定,证明CO_2气体为火山冷凝后释放出来的。
This paper states the geological conditions of the formation of mineral water at the five linking lakes the formation process of the CO_2 gas in mineral water and its evolution tendency. Based on the determination of isotopes ^(13)C, ^(18)O etc., it is proved that the CO_2 comes from the releasing of gases at the volcano cooling condensation.
出处
《勘察科学技术》
1991年第6期11-13,共3页
Site Investigation Science and Technology
