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    Neoproterozoic Arc - related mafic intrusions along the Northern Margin of South China: implications for accretion of Rodinia

    120016_11209_Neoproterozoic - Journal of Geology.pdf (431.3Kb)
    Access Status
    Open access
    Authors
    Zhou, M.
    Kennedy, Allen
    Sun, M.
    Malpas, J.
    Lescher, C.
    Date
    2002
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Zhou, Mei-fu and Kennedy, Allen and Sun, Min and Malpas, John and Lescher, Chris. 2002. Neoproterozoic Arc - related mafic intrusions along the Northern Margin of South China: implications for accretion of Rodinia. Journal of Geology. 110 (5): pp. 611-618.
    Source Title
    Journal of Geology
    DOI
    10.1086/341762
    ISSN
    00221376
    Faculty
    Department of Medical Imaging and Applied Physics
    School of Science
    Science and Engineering
    Remarks

    The link to the journal's home page is: http://www.journals.uchicago.edu/toc/jg/current

    Copyright © 2002 University of Chicago Press. All rights reserved.

    URI
    http://hdl.handle.net/20.500.11937/31454
    Collection
    • Curtin Research Publications
    Abstract

    South China has been considered as part of the Rodinian supercontinent during Neoproterozoic time, although itspaleogeographic position within this supercontinent is still a matter of debate. The Wangjiangshan and Bijigou complexesalong the northern margin of South China are among the largest mafic intrusions in China. New SHRIMPzircon U-Pb results indicate that these two intrusions have crystallization ages of 820 Ma and 780 Ma, respectively.Enrichment of large ion lithophile and light rare earth elements and depletion of high field-strength elements in theseintrusions suggest derivation from an active arc along a continental margin. This interpretation of these intrusionsas part of a continental arc assemblage is in contrast with the previous view that they were products of a Neoproterozoicmantle plume that initiated the breakup of Rodinia. The presence of a Neoproterozoic magmatic arc suggests thatRodinian oceanic lithosphere was subducted beneath the (present) northern margin of South China and therefore thatSouth China flanked the Rodinian ocean.

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