地洼学说基本理论的形成与发展

地洼学说是由著名地质学家陈国达教授创立的。从创立至今,经过我国及其他一些国家地质工作者的长期辛勤劳动,使之日臻完善,并形成了在国内外有影响的地质科学理论。近35年的实践证明,这一理论对生产实践具有重要的指导作用。地洼学说的形成,是陈国达教授应用科学的思想方法在地质科学道路上大胆创新、不断探索的结果。地质工作所涉及的研究领域非常广泛而复杂,它更需要科学的、系统的理论来指导。我们学习和研究地洼学说的形成过程和创新精神,除了它的应用价值外,其理论意义特别是科学的思想方法也是值得我们很好学习和借鉴的。

The Origin and Development of the Essentials of Diwa Theory

diwa theory was developed by professor Chen Guoda, the famous geologist alive in China. Through diligence and harworking, geologists both in China and abroad have brought the theory to completion and made it an influential geological theory. For thirtyfive years of implementation, this theory has proved to be significant in productive practice. However, diwa theory is accepted to be of great value not only in practical appli- cation but also in fashion of scientific thinking.