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The Nd-Sr isotope study of Mesozoic granitoids in Jiangxi Province

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Chinese Science Bulletin

Abstract

Nd-Sr isotopic compositions of 12 Mesozoic granitoids from Jiangxi Province have been reported. They show low-∈ND(−13.8–−8.3), high-/Sr(0.71069–0.73981) and oldt DM (2087–1635 Ma). Comparison between the Sm-Nd isotopic compositions of the granitoids and those of the basement metamorphic racks suggests that these granitoids were mainly derived from the metasedimentary rocks. There is an east-west trend Mesozoic granitoid zone with low-tDM from S. Jiangxi to S. Fujian. The origin of these granites was preliminarily discussed.

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Authors and Affiliations

  1. Department of Earth Sciences & State Key Laboratory of Mineral Deposit Research, Nan**g University, 210093, Nan**g, China

    Weizhou Shen, Hongfei Ling, Wuxian Li & Dezi Wang

  2. Institute of Geology, Chinese Academy of Sciences, 100029, Bei**g, China

    Xuan Huang & Jun Pan

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  1. Weizhou Shen
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  2. Hongfei Ling
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  3. Wuxian Li
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  4. Dezi Wang
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  5. Xuan Huang
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  6. Jun Pan
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Shen, W., Ling, H., Li, W. et al. The Nd-Sr isotope study of Mesozoic granitoids in Jiangxi Province. Chin.Sci.Bull. 44, 1427–1431 (1999). https://doi.org/10.1007/BF02885998

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  • DOI: https://doi.org/10.1007/BF02885998

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