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建国以来,根据不断积累的大量实际地质资料,我们对中国大地构造的特点,曾经不断地进行过分析研究,并先后发表了一些论文。现在将我们的最近成果和见解简短地阐述如下,供广大地质工作人员参考。一、欧洲和苏联地质学家的单旋回观点简介(图1) 1939—1950年间史蒂勒发表了几篇论文,提出地槽褶皱带的构造岩浆旋回发展特点,并总结如下表:
Since the founding of the People’s Republic of China, based on the continuous accumulation of a large amount of actual geologic data, we have continuously conducted analytical studies on the characteristics of the geotectonic structure of China and successively published some papers. We will now briefly explain the recent achievements and insights below, for the general geological staff reference. I. Introduction to single-cycle views of geologists in Europe and the Soviet Union (Figure 1) Stiller published several papers from 1939 to 1950 and proposed the tectonic magmatic gyration characteristics of the geosynclinal fold belt. The summary is as follows: