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磷矿是最重要的农肥矿物原料,它对提高农作物单位面积产量有着重要的作用。中国科学院地貭研究所对磷矿的研究,虽然在1956年即曾进行了一些零星的工作,但正式工作却是在1958年的大跃进中开始的。当时我們分析了中国磷矿资源的現状,发現其中最主要的問題是地区不平衡,首先应在华北广大农业地区找出磷矿。要解决这个問题,第一、要明确到那里去找,第二、要拟定怎样才能在最短的时間內取得成果的工作方法。当时我們信为,要解决到那里去找的問題,就必須掌握切合中国实际地貭情况的成矿理論,有了成矿理論的指导,然后就能有方向。于是我們决定先摸成矿理論,再进行找矿。在我們研究了已有的不同成矿理論,拟定了我們的工作假說之后,便馬上出发到各个已有的矿点去实践和驗証。由于事先有准备,心中有数,我們对成矿理論的研究在短短的时間內得到了不少成果。但时間究竟过去了不少,当我們考虑到北
Phosphate rock is the most important raw material of agricultural fertilizer and mineral fertilizer, and it plays an important role in improving yield per unit area of crops. The research on phosphate rock by the Institute of Groundwater Science and Technology, Chinese Academy of Sciences, started some sporadic work in 1956, but formal work started in the Great Leap Forward in 1958. At that time, we analyzed the status quo of phosphate rock resources in China and found that the most important problem was the imbalance in the region. First, we should find phosphate rock in the vast agricultural areas in North China. To solve this problem, the first is to find out exactly where to go and the second is to formulate a working method of how to achieve results in the shortest possible time. At that time, we believed that in order to solve the problem of going there, we must master the metallogenic theory that meets the actual situation in China. With the guidance of metallogenetic theory, we can have direction. So we decided to touch the theory of mineralization, then prospecting. After we studied the existing different mineralization theories and formulated our working hypothesis, we immediately set off to each existing mine site to practice and verify. Due to the preparation beforehand and the fact that we know it, our research on the metallogenic theory has yielded many achievements in a short period of time. But the time has passed a lot when we consider North