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陈国达教授于1956年提出地洼学说后,受到国内外的高度重视,被列为自然科学史上的大事之一(《自然科学大事年表》,上海人民出版社,1975)。有的国家作为新的找矿理论和科研方向,加以发展,正逐步形成一个以我国为起源的国际性学派。 近年来,国内外学者从不同的角度来研究地洼学说及其成矿理论,有的研究作为地洼学说的核心的递进思想的形成及其哲学意义等。 应各方面地质工作者的要求,为了使广大读者对陈国达教授学术思想的发展历程,地洼学说的孕育、形成和发展及其实践依据,特就资料所及,将他的历年著作,包括五
After Professor Chen Guoda put forward the theory of diwa in 1956, he was highly regarded both at home and abroad and was listed as one of the major events in the history of natural science (Chronology of Natural Sciences, Shanghai People’s Publishing House, 1975). Some countries, as the new prospecting theory and research direction, have been developed and are gradually forming an international school with China as its origin. In recent years, scholars at home and abroad have studied Diwa theory and its metallogenic theory from different perspectives, while others have studied the formation and philosophical significance of progressive thought as the core of Diwa theory. In response to the request of geologists at all levels, in order to enable readers to study the development course of Professor Chen Guoda’s academic thoughts, the birth, formation and development of Diwa and its practical basis,