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  1. 1
    Early Permian post-collisional high-K granitoids from Liuyuan area in southern Beishan orogen, NW China: Petrogenesis and tectonic implications

    Early Permian post-collisional high-K granitoids from Liuyuan area in southern Beishan orogen, NW China: Petrogenesis and tectonic implications by Li, S., Wilde, Simon, Wang, T.

    Published 2013
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  2. 2
    Neoarchean siliceous high-Mg basalt (SHMB) from the Taishan granite–greenstone terrane, Eastern North China Craton: Petrogenesis and tectonic implications

    Neoarchean siliceous high-Mg basalt (SHMB) from the Taishan granite–greenstone terrane, Eastern North China Craton: Petrogenesis and tectonic implications by Touping, P., Wilde, Simon, Weiming, F., Bingxia, P.

    Published 2013
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  3. 3
    The 825 Ma Yiyang high–MgO basalts of central South China: Insights from Os–Hf–Nd data

    The 825 Ma Yiyang high–MgO basalts of central South China: Insights from Os–Hf–Nd data by Wu, T., Wang, Xuan-Ce, Li, W., Wilde, Simon, Tian, L., Pang, C., Li, J.

    Published 2018
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  4. 4
    Intraplate crustal remelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong Province, SE China

    Intraplate crustal remelting as the genesis of Jurassic high-K granites in the coastal region of the Guangdong Province, SE China by Huang, Hui-Qing, Li, X., Li, Zheng-Xiang, Li, W.

    Published 2013
    “…They are high in K2O (3.5–7.0 wt%) and K2O/Na2O (>1), and have trace element concentrations (e.g., Nb, Y, Zr and Ga) similar to typical I-type granites in the Lachlan Fold Belt, southeastern Australia. Their whole-rock ISr (0.7057–0.7077) and εNd(t) (−6.46 to −3.13) are less evolved than many coeval granites in this region. …”
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