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岩浆热液型铅锌矿床是我国要重矿产资源之一。它与中酸性浅成超浅成小侵入体活动密切相关,而且多产于岩体与碳酸盐岩地层接触带及其附近的地方。研究其形成条件对铅锌矿床的找矿具有重大意义。 对岩浆热液型铅锌矿床进行较为系统实验研究尚未见报导,但就这类矿床中的各个侧面进行单项研究的人很多(见参考文献)。我们的实验在国内外前人研究基础上,对发育在围岩的断裂,破碎带的岩浆热液矽卡岩型铅锌矿及铁铅锌多金属矿床的主要成矿过程作了一个简单的系统实验研究。
Magmatic hydrothermal lead-zinc deposits are one of the most important mineral resources in China. It is closely related to the activity of moderate-acid shallow and ultra-shallow into small intrusions, and it is prolific in the contact zone of rock mass and carbonate formation and its vicinity. It is of great significance to study the formation conditions of prospecting for lead-zinc deposits. Systematic experimental studies on magmatic hydrothermal Pb-Zn deposits have not been reported, but many studies have been conducted on each side of this type of deposit (see references). Based on the previous studies both at home and abroad, our experiments have made a brief introduction to the major mineralization processes of the magmatic hydrothermal skarn-type lead-zinc deposits and iron-lead-zinc polymetallic deposits that are developed in the fractured and fractured zones of the surrounding rocks System experiment research.