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Re-Os isotope geochemistry of three Chinese chondrites
作者姓名:ZHI  XiaChen  QIN  Xie  SHI  RenDeng  HONG  JiAn
作者单位:CAS Key Laboratory of Crust-Mantle Material and Environment, School of Earth and Space Sciences, University of Science andTechnology of China, Hefei 230026, China
基金项目:Supported by the National Natural Science Foundation of China (Grant No. 40473008 and 40572036)
摘    要:Three Chinese ordinary chondrites,including Jilin (H5),Boxian (LL3.8) and Lujiang (LL6),have been studied for their Re and Os abundances and Os isotopic composition in whole-chondrite samples,separated magnetic and nonmagnetic fractions,and nodules. The results indicate that the Re and Os abundances of the whole-chondrite samples are in the ranges of corresponding H-and LL-Groups,respectively. The Re and Os abundances of magnetic fraction from Boxian and Lujiang are within the range of high-Os ⅡAB and ⅢAB irons,whereas those of nonmagnetic fractions of Boxian and Lujiang are lower than the whole-chondrite values. The Re and Os abundances of nodules in Jilin are in the range of the LL-Group. 187Re/188Os and 187Os/188Os ratios of the three whole chondrites are in the range of ordinary chondrites which locate around the isochron of ⅡAB ⅢAB irons. 187Re/188Os and 187Os/188Os ratios of the magnetic and nonmagnetic fractions from Boxian have a larger difference. The nonmag-netic fraction of Lujiang may contain a recent addition of Re,which causes deviation of the 187Re/188Os ratio from the irons isochron. The Re and Os abundances of nodules in Jilin are lower than those of the whole-chondrite,but their 187Os/188Os ratios are higher than that of the whole chondrite.

关 键 词:球粒状陨石      同位素地球化学  中国
收稿时间:9 December 2006
修稿时间:2006-12-09

Re-Os isotope geochemistry of three Chinese chondrites
ZHI XiaChen QIN Xie SHI RenDeng HONG JiAn.Re-Os isotope geochemistry of three Chinese chondrites[J].Chinese Science Bulletin,2007,52(16):2269-2274.
Authors:Zhi XiaChen  Qin Xie  Shi RenDeng  Hong JiAn
Institution:(1) CAS Key Laboratory of Crust-Mantle Material and Environment, School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China
Abstract:Three Chinese ordinary chondrites, including Jilin (H5), Boxian (LL3.8) and Lujiang (LL6), have been studied for their Re and Os abundances and Os isotopic composition in whole-chondrite samples, separated magnetic and nonmagnetic fractions, and nodules. The results indicate that the Re and Os abundances of the whole-chondrite samples are in the ranges of corresponding H-and LL-Groups, respectively. The Re and Os abundances of magnetic fraction from Boxian and Lujiang are within the range of high-Os IIAB and IIIAB irons, whereas those of nonmagnetic fractions of Boxian and Lujiang are lower than the whole-chondrite values. The Re and Os abundances of nodules in Jilin are in the range of the LL-Group. 187Re/188Os and 187Os/188Os ratios of the three whole chondrites are in the range of ordinary chondrites which locate around the isochron of IIAB+IIIAB irons. 187Re/188Os and 187Os/188Os ratios of the magnetic and nonmagnetic fractions from Boxian have a larger difference. The nonmagnetic fraction of Lujiang may contain a recent addition of Re, which causes deviation of the 187Re/188Os ratio from the irons isochron. The Re and Os abundances of nodules in Jilin are lower than those of the whole-chondrite, but their 187Os/188Os ratios are higher than that of the whole chondrite. Supported by the National Natural Science Foundation of China (Grant No. 40473008 and 40572036)
Keywords:Re and Os abundances  Re-Os isotopes  ordinary chondrites
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