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新中国成立以来的三十一年中,金属矿床地质规律的研究经历了从低级趋向高级的过程.五十年代是描述阶段,积累了大量的原始写实资料;六十年代转入分地区、分矿种、分类型的归纳、对比和综合研究阶段,总结出了一些矿床的地质规律、找矿标志和找矿方向,直到目前这个阶段仍在继续.不过,从七十年代后期起,地质科研工作呈现出向新阶段过渡的状态.标志这种状态的是在金属矿床地质研究中日益重视两个方面:一个是“定性转向定量”,即广泛使用各种物理、化学方法手段来提供数据、图象以补充或代替定性概念,用相对更确切、正确的数据来代替原先不太确切、正确或半定量的数据,开展实验方法来模拟地球内部的成矿作用,用数理统计的科学概念代替因人而异的地质观察概括印象等等;另一个是“感
During the thirty-one years since the founding of New China, the study on the geological laws of metal deposits has undergone a process from low to high, with the fifties describing the stage and accumulating a large amount of original realistic material. In the 1960s, Mineralization, classification of the induction, comparison and comprehensive research stage, summed up some of the geological laws of ore deposits, prospecting signs and prospecting direction, until now this stage is still continuing.However, since the late seventies, geological research The work shows a state of transition to a new phase, which is marked by the growing emphasis in geological research on metal deposits in two aspects: one is “qualitative diversification”, that is, a wide range of physical and chemical methods are used to provide data, Like complementing or substituting qualitative concepts, replacing less accurate, correct or semi-quantitative data with relatively more accurate and correct data, conducting experimental methods to simulate the mineralization within the Earth, and substituting scientific notions of mathematical statistics for Geological observations of different people summarize the impression and so on; the other is "feeling