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Suizhou Meteorite: Mineralogy and Shock Metamorphism pp 211–223Cite as

Shock-Induced Redistribution of Trace Elements

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Abstract

The statistics of mineral contents in the Suizhou meteorite gives the following results (in volume %): olivine-44, pyroxene-31, plagioclase-14, opaque minerals (FeNi metal, troilite, and chromite)-10, and whitlockite-1 (Zeng 1990).

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References

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Authors and Affiliations

  1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, Guangdong, China

    Xiande Xie & Ming Chen

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  1. Xiande Xie
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  2. Ming Chen
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Correspondence to Xiande Xie .

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© 2016 Springer-Verlag Berlin Heidelberg and Guangdong Science & Technology Press Co., Ltd.

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Xie, X., Chen, M. (2016). Shock-Induced Redistribution of Trace Elements. In: Suizhou Meteorite: Mineralogy and Shock Metamorphism. Springer Geochemistry/Mineralogy. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-48479-1_6

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