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《Northwest Geoscience》 1991-02
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Zhang Ruilin (Xi'an Institute of Geology and Mineral Resources, CAGS)  
In the course of studying the tectonic evolution in the QinglingDabashan region, the author gradually realizes that the evolution and paleoenvironment at all stages of the region, which is located between North China and Yangtze blocks, depended on their relative locations and interrelation. For this purpose, author collects a lot of North China and Yangtze open published paleomagnetic data which can serve as important mean for the investgation of plate activities. On the basis of calculation, sorting out and analysis of there data, and combrised with the reference of rich geological materials from all parts of the region, the development and evolotion between the blocks from Sinian to Tertiary Period is then divided into three stages: the late Sinian to Silurian active stage, the late Silurian to Late Triassic intesrestucted stage and the Late Triassic to Tertiary stable stage. From the above-classification, author can abtain three corresponding developing stages of the region, i. e. the oceanic crust to continental crust developing stage, the pulling-apart to downrifting to contraction stage of the continental crust, and the solidification and up rise stage of the continent.
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Chinese Journal Full-text Database 3 Hits
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