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《Progress In Precambrian Research》 2001-01
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U-Pb Single Zircon Ages for Granulites in Cunkongshan Area, Guyang Inner Mongolia and Enlightenment for It's Geological Signification, China

WANG Hui chu, YUAN Gui bang, XIN Hou tian (Tianjin Institute of Geology and Mineral Resources, Tianjin China 300170)  
There is a suit of granulite-facies metamophic supracrustal rocks in Cunkongshan area, Guyang, Inner Mongolia, from which two sample have been collected. The metamorphic supracrustal rocks in Yangtaigou from which sample No.P7JD4-25 Was obtained occurred as enclave in tonalite-gneiss, and in Heilongdong from which sample No. HL-5 was collected occurred as massive enclave in charnockite-gneiss. The zircons from former No.P7JD4-25 yield an up intercept age of (2 503±20)Ma which is consistent with the age from tonalite-gneiss. And yet the zircons from No. HL-5 yield an up intercept age of (2 648.5±5)Ma、 a 207 Pb/ 206 Pb age of (2 673±8)Ma and other ages of (2 450~2 510)Ma, the former two were interpreted as the age of granulite-facies metamorphicl event, and the later has similar meaning with No. P7JD4-25's. The age of (2 648.5±5)Ma and a 207 Pb/ 206 Pb age of (2 673±8)Ma were the greatest age which have been obtained so far using the method of single zircon from west-central part of Inner mongolia (include northern Shanxi and west-northern Hebei). It is important for the research about the precambrian crustal evolution of margin of North China.
【Fund】: 国家地质大调查项目! (J4 .1.2 )
【CateGory Index】: P597
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