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《》 1987-05
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Yang Weiran (Wuhan College of Geology, Wuhan 430074)  
East Qinling lies between North China old land and Yangtze old land. Its tectonic evolution is essentially the history of continuous opening-closing of the two old lands. In the light of opening-closing characteristics, four stages can be divided. 1. Mid-late proterozoic plate subduction-convergence stage. 2. Paleozoic fault orogenic belt formation stage. 3. Early Mesozoic fault block mobilization stage. 4. Late Mesozoic-Cenozoic fault basin development stage.
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