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本文在综合整理研究各种天然水化学成分资料的基础上指出,一些重要的现代含矿溶液(如红海、索尔顿海、密西西比中部、切列肯等处)与岩浆水在成分上明显不同,其SO_4~(2-)Cl~-与HCO_3~-Cl~-值均<0.01,可称为高纯氯化物卤水。据产于火山口或火山锥上的一些火山热泉资料分析判断,其中不存在高纯氯化物水。在我们所知的一些火山射气分析资料中亦不存在持续的高纯氯质射气。雷德尔汇集的火成岩中气液包裹体成分资料也是如此。因而可以
Based on a comprehensive review of various natural water chemical composition data, it is pointed out that some important modern ore-bearing solutions (such as the Red Sea, the Salton Sea, central Mississippi, Chereken, etc.) are significantly different in composition from magmatic water , The SO_4 ~ (2-) Cl ~ - and HCO_3 ~ -Cl ~ - values ?? are less than 0.01, can be referred to as high purity chloride brine. According to some volcanic hot springs produced in crater or volcano cone data analysis and judgment, which does not exist in high purity chloride water. There are also no persistent high-purity chlorine-based projectiles in some of the volcanic gas analyzes that we know. The same is true of information on the composition of gas-liquid inclusions in igresides from Riddle. So you can