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《Acta Geosicientia Sinica》 2003-06
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Pb-Sr-Nd-O Isotope Characteristics of Granitoids in East Kunlun Orogenic Belt

LIU Chengdong 1,2) MO Xuanxue 1) LUO Zhaohua 1) YU Xuehui 1) CHEN Hongwei 1) LI Shuwei 1) ZHAO Xin 1) ( 1)China University of Geosciences,Beijing,100083; 2)East China Institute of Technology,Fuzhou,Jiangxi,344000)  
This paper reports Pb, Sr, Nd and O isotopic compositions of gabbro and granitoids formed in East Kunlun orogenic belt in Triassic. Granitoids and potassic feldspar have similar Pb isotopic compositions. Studies show that they were formed in an orogenic environment.Initial ( 87Sr/ 86Sr)t ratios range from 0.70144 to 0.70972,and εNd values from -4.49939 to -9.19258. Nd isotopic model ages (t DM) vary from 1.38 Ga to 1.761 Ga, being close to the age of mesoproterozoic metamorphic rocks. O isotopic compositions range from 7.8 to 9.5, indicating that the granitoids were derived from the crust. Based on all isotope data and mineralogical as well as petrochemical studies, it is held that the granitoids were mainly derived from the crust and mixed with the mantle-derived materials. The mixing process between the crust materials and the mantle-derived materials is responsible for the nearly identical isotope compositions.
【Fund】: 中国地质调查局重点项目“花岗岩重大地质问题研究”(编号 2 0 0 113 90 0 0 18);; 国家重点基础研究发展规划项目 (G19980 40 80 0 2 0 0 2CB412 60 0 )资助
【CateGory Index】: P597
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