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    Confirming of the Heilongjiang ~500Ma Pan-African khondalite belt and its tectonic implications

    Access Status
    Fulltext not available
    Authors
    Zhou, Jian-bo
    Zhang, X.
    Wilde, Simon
    Zheng, C.
    Date
    2011
    Type
    Journal Article
    
    Metadata
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    Citation
    Zhou, J. and Zhang, X. and Wilde, S. and Zheng, C. 2011. Confirming of the Heilongjiang ~500Ma Pan-African khondalite belt and its tectonic implications. Acta Petrologica Sinica. 27 (4): pp. 1235-1245.
    Source Title
    Acta Petrologica Sinica
    ISSN
    10000569
    URI
    http://hdl.handle.net/20.500.11937/45718
    Collection
    • Curtin Research Publications
    Abstract

    The basement rocks in NE China, including Mushan Group in Jiamusi Block, Xinghuadukou Group in the Xing' an Block, constitute a khondalitic sequence of sillimanite- and garnet-bearing gneisses, hornblende-plagioclase gneiss and felsic paragneisses. Zircon U-Ph dating of the garnet-sillimanite gneiss samples from Erguna, Xing' an and Khanka blocks indicates high-grade metamorphism occurred at similar to 500Ma, where several detrital zircon grains whose ages extend between 600Ma to 850Ma. The Pan-African high-grade metamorphism with magmatism events were obtained from all the blocks in NE China, including the Erguna, Xing' an, Songliao and Jiamusi-Khanka blocks, establish a over 1300km Pan-African khondalite belt in NE China, named here the Northeast China Khondalite Belt'. The results from this study provide new idea for researching the tectonic affinity and plate evolution in the NE...

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