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卤水成矿学说目前颇为流行.这种学说把密西西比河谷型矿床和现在正在沉积的红海、索尔顿海等海底发现的多金属沉积物联系在一起,认为它们是含矿卤水在不同空间,不同成矿方式的表现.下面就卤水成矿的几个基本问题作一扼要分析.由于水平所限,对各种资料分析、归纳不一定合适,望批评指正.卤水的来源含盐度大于5%的天然水体称为卤水.卤水在地壳中分布是比较广泛的.除火山热泉卤水外,根据地层卤水中盐分的来源,大
Brine mineralization theory is quite popular at present, which links the Mississippi valley deposit with the polymetallic deposits found on the seabed of the Red Sea and the Salton Sea which are now being deposited, and considers them to be ore-bearing brines in different spaces, Different metallogenic ways.The following is a brief analysis of several basic problems of mineralization of the brine.Because of the limited level, it is not necessarily suitable to analyze and summarize all kinds of data.It is expected that the salinity of brine will be more than 5 % Of natural water known as the brine. Brine distribution in the crust is more extensive. In addition to volcanic hot spring brine, according to the brine source brine, large