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矿床的形成是属于地下深部岩浆活动过程?还是属于海洋表层的地球化学活动过程?这不仅关系到探查地下资源的基本战略,而且也是左右着认识整个地球史的重要问题。我通过对黑矿成因论的重新研究,从而认识到地球上的矿床,从其本质上都可说是海洋地球化学作用的产物。黑海和挪威峡湾等处成层水系的地球化学研究结果,弄清了“溶存氧”的消失边界(O_2—H_2S边界)中重金属元素明显的氧化与还原的实际情况。这就是以Cu、Zn、Pb等为代表
The formation of the deposit belongs to the deep underground magmatic activity or the geochemical activity of the ocean surface? This is not only related to the basic strategy of exploring underground resources, but also an important issue that affects the entire earth history. Through a re-study of the genesis of black ores, I realized that deposits on earth are, by their nature, products of ocean geochemistry. Black Sea and Norwegian fjords stratified aquifer geochemical results of the study to clarify the disappearance of dissolved oxygen (O_2-H_2S boundary) of heavy metals in the obvious oxidation and reduction of the actual situation. This is represented by Cu, Zn, Pb and so on