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数年前,中国地质科学院编制并出版了五百万分之一的亚洲地质图和四百万分之一的中国大地构造图。在此基础上,我们用板块构造理论编制了八百万分之一的亚洲大地构造图。由于古老板块构造遗迹常遭到后期构造的破坏,不易辨认。所以我们追溯亚洲的板块活动将自显生宙开始。由于在亚洲震旦系或上元古界常与古生代地层平行叠覆,所以实际上古板块的活动是从震旦纪或晚元古代开始的。在不同时期各板块之间随时都有变化。用一幅图勾绘各地质历史时期的板块分布范围是困难的。但为说明亚洲板块构造的发展,兹姑作一个简单的划分。并就所遇到的问题,提出讨论。
A few years ago, the Chinese Academy of Geological Sciences prepared and published a map of Asia in five millionths of Asia and four millionths of China. Based on this, we constructed the tectonic map of the Asian continent in 8,000,000th parts using plate tectonics theory. Due to the ruins of the ancient plate tectonics were often destroyed by the late structure, not easy to identify. Therefore, the activities of our plate traced back to Asia will start from the Inner Mongolia. Due to the fact that the Sinian or Upper Proterozoic in Asia often overlaps the Paleozoic strata in parallel, the activity of the ancient plate actually started in the Sinian or Late Proterozoic. In different periods between the plates have changed at any time. It is difficult to plot the distribution of plates in all geologic historical periods with a picture. However, to illustrate the development of plate tectonics in Asia, it is easy to make a simple division. And discuss the problems we encountered.