ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
黄土高原黄土和太平洋沉积物 Nd,Sr 同位素变化的比较
  
关键词:Nd and Sr isotopes colian deposits loess plateau
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杨杰东 南京大学现代分析中心江苏 南京210093南京大学成矿机制研究国家重点实验室江苏 南京210093 jdyang@nju.deu.cn 
陈骏 南京大学地球科学系江苏 南京210093  
张兆峰 南京大学地球科学系江苏 南京210093  
季峻峰 南京大学地球科学系江苏 南京210093  
陈旸3) 南京大学地球科学系江苏 南京210093  
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摘要:
A Comparison of Variations in Nd and Sr Isotopic Compositions between the Loess Plateau and the Pacific Sediments
      143Nd/144Nd and 87/Sr/86Sr rations of acid-washed residues of red clay and overlying loess-paleosols from the Lingtai profile in the loess plateau of China were determined. Sediments in central North Pacific Ocean have different fluctuations fo 87Sr/86Sr ratios from the Lingtai profile over the last 7.0 Ma. Nevertheless, fluctuations of ENd(0) in the Lingtai Profile from 7.0 Ma B P to the present are very similar to those of central North Pacific Ocean, which reflects the loess of the less plateau in China and sediments of central North Pacific Ocean are derived from the same source regions, and the source regions have been basically unchnged since 7.0 Ma B P. Red clay and the overlying loess-paleosol have very identical ENd (0). It can be inferred that both the red clay in the Loess Plateau and the overlying loess-paleoaols are probably of eolian origin and have the same source region. The phenomenon that most of the residues of red clay have higher 87Sr/86Sr ratios than the overlying loess-paleosols implies a climate of relatively high tempera ture and strong rainfall during the formaion of red clay.
YANG Jiedong,CHEN Jun,ZHANG Zhaofeng,JI Junfeng,CHEN Yang.2005.A Comparison of Variations in Nd and Sr Isotopic Compositions between the Loess Plateau and the Pacific Sediments[J].Acta Geoscientica Sinica,26(z1):192-194.
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