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    Ca. 1.5 Ga mafic magmatism in South China during the break-up of the supercontinent Nuna/Columbia: The Zhuqing Fe–Ti–V oxide ore-bearing mafic intrusions in western Yangtze Block

    Access Status
    Fulltext not available
    Authors
    Fan, H.
    Zhu, W.
    Li, Zheng-Xiang
    Zhong, H.
    Bai, Z.
    He, D.
    Chen, C.
    Cao, C.
    Date
    2013
    Type
    Journal Article
    
    Metadata
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    Citation
    Fan, Hong-Peng and Zhu, Wei-Guang and Li, Zheng-Xiang and Zhong, Hong and Bai, Zhong-Jie and He, De-Feng and Chen, Cai-Jie and Cao, Chong-Yong. 2013. Ca. 1.5 Ga mafic magmatism in South China during the break-up of the supercontinent Nuna/Columbia: The Zhuqing Fe–Ti–V oxide ore-bearing mafic intrusions in western Yangtze Block. Lithos. 168-169: pp. 85-98.
    Source Title
    Lithos
    DOI
    10.1016/j.lithos.2013.02.004
    ISSN
    0024-4937
    URI
    http://hdl.handle.net/20.500.11937/48216
    Collection
    • Curtin Research Publications
    Abstract

    Secondary ion mass spectroscopy (SIMS) zircon and baddeleyite U–Pb ages, elemental, and Nd isotopic data are reported for the Zhuqing Fe–Ti–V oxide ore-bearing mafic intrusions in western Yangtze Block, South China. The mafic intrusions are dated at 1494±6 Ma (zircon U–Pb), 1486±3 Ma (baddeleyite U–Pb) and 1490±4 Ma (baddeleyite U–Pb). The intrusions are dominantly gabbros that experienced variable degrees of alteration. All the studied rocks are high-Ti and alkaline in composition, and exhibit light rare earth element enrichment and “humped” incompatible trace-element patterns with no obvious Nb–Ta depletion, similar to intraplate alkali basaltic rocks in continental flood basalt (CFB) and ocean island basalt (OIB) provinces. Negative εNd(T)values (-0.97 to -3.58) and fractionation of the HREE of these rocks indicate that they were derived from a time-integrated, slightly enriched asthenospheric mantle source with minor crustal contamination. Like other Fe–Ti oxide mineralized rocks in plume-related layered intrusions or large igneous provinces around the world, the Zhuqing gabbros likely occurred in an intraplate setting. The ~1.5 Ga mafic magmatism was likely part of the global 1.6–1.2 Ga anorogenic magmatism related to the break-up of the supercontinent Nuna/Columbia, suggesting that the Yangtze Block may have been a component of the supercontinent.

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