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《Journal of Jilin University(Earth Science Edition)》 2009-03
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Zircon U-Pb Age and Geological Significance of the Taizili Granitic Gneiss from Western Liaoning Province

ZHENG Pei-xi1,JIN Wei1,ZHOU Yan2,LI Jian1,ZHENG Chang-qing11.College of Earth Sciences,Jilin University,Changchun 130061,China2.Center of Analysis and Testing,Jilin University,Changchun 130026,China  
A suit of rock association of granitic gneiss and supracrustal xenoliths,described as the Dayingzi Formation,Jianping Group previously,is widely distributed in the Taizili area in western Liaoning Province.During the research of recent year,the Dayingzi Formation,Jianping Group was disintegrated into granitic plutonic gneiss and layered rock series.This granitic gneiss has similar features as those in the Yebaishou and the Caojiashaoguo gneiss in Dayingzi area.The granitic gneiss could represent the important Archean magma event in western Liaoning Province.The LA-ICP-MS dating method of single particle zircon of granitic gneiss suggests its magma emplacement age is about 2 522 Ma,an significance geological event in the western Liaoning Province.This dating also gives some chronological information for the Late Archean continental crust accretion event in the area.
【Fund】: 国家油气专项(XQ2004-07);; 中石化海相前瞻性项目(G0800-06)
【CateGory Index】: P588.345
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9 WU Fu-yuan~(1,2), GE Wen-chun~2, SUN De-you~2, GUO Chun-li~2(1.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100101,China;2.College of Earth Sciences, Jilin University, Changchun 130061,China);DISCUSSIONS ON THE LITHOSPHERIC THINNING IN EASTERN CHINA[J];Earth Science Frontiers;2003-03
10 LI Jin-yi~1, MO Shen-guo~(1,2), HE Zheng-jun~1, SUN Gui-hua~1, CHEN Wen~1(1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. State key laboratory of Resources and Environment Information System, Institute ofGeographic Sciences and Natural Resources Research, CAS, Beijing 100101, China);The timing of crustal sinistral strike-slip movementin the northern Great Khing'an ranges and its constrainton reconstruction of the crustal tectonic evolution ofNE China and adjacent areas since the Mesozoic[J];Earth Science Frontiers;2004-03
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