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《Acta Scicentiarum Naturalum Universitis Pekinesis》 1991-02
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The Zircon U-Pb Ages of Archean Metamorphic Rocks in Western Liaoning Province-Chifeng Area

CUI Wenyuan, WANG Changqiu (Department of Geology, Peking University)SUN Chengzhi, ZHANG Yuye (The Third Geological Team of Inner Mongolia)  
The area studied is situated in 41°15′-42°30′N and 118°00′-121°00′E, belongs to the northern part of North China Platform and the eastern part of Inner · Mongolia geoaxis. Archean metamorphic rocks are mainly distributed in three parallel uplifts of NE direction. From east to west, they are Nulu'erhu uplift, Qilaotu uplift and Yun-wushan uplift. According to the metamorphic rock assemblages and their characteristics, Whole Archean metamorphic rocks can be subdivided into Jianping Complex and Dayingzi Croup.The U-Pb zircon method has been applied to dating metamorphic rocks in this area. Based on the four U-Pb zircon results, conbined with geological features of this area, conclusions have been made, as follows-1. Zircon discordant dating for the samples 8H3 and 811 give the ages of 2575 and 2579 Ma. They are interpreted as the formation.2. Zircon discordant dating for the samples 7Y138 and 8D182 give the ages of 2481 Ma. They can be interpreted as ages for Late Archean metamorphic event which may be correlated with the same event recognized in the Qianxi Group, eastern Hebei.3. The age of protolith of metamorphic rocks in this area should be older than 2500 Ma.4. The metamorphic rocks in three uplifts should have similar evolution history before 2500 Ma.
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