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《GEOLOGY OF ANHUI》 1999-03
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THE ISOTOPIC AGE OF THE JINGSHAN INTRUSIVEIN THE BENGBU REGION OF THE SOUTHEASTERN EDGEOF THE NORTH CHINA BLOCK AND ITS GEOLOGICAL IMPLICATIONS

Qiu Ruilong, Xu Xiang, Huang Dezhi(Anhui Academy of Geological Survey, Hefei 230001,China)  
A suit of granite rocks that widely spread in the Bengbu region of the southeastern edge of the North China Block have for a long time been regarded as mixed granites formed in the Bengbu stage of the Archean, which, however, is not supported by the data acquired in the recent years, which indicate that the rocks have characteristics of magmatic intrusion and differential evolution in veiw of either their rock type association and texture or the intrusive contact relationship between them and wall rocks, especially the 40Ar-39Ar isotopic age of biotite from the Jingshan biotite adamellite that definitely demonstrates the existence of magmatic activity of early Yanshanian stage of the Mesozoic in the region
【CateGory Index】: P597
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