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[21]王炯辉, 马星化, 李毅, 陆灿友, 陈凌云, 陈斌, 王志强, 2014. 花岗质复式岩体成因及其与W-Mo成矿的关系—以广西油麻坡岩体为例. 地质学报, 88: 1219-1235.
[22]马星华, 陈斌*, 王志强, 高林, 孙克克, 2014. 南岭连阳复式岩体成因: 锆石U-Pb年代学、地球化学和Nd-Hf同位素约束. 地学前缘, 21: 264-280.
[23]马星华*, 王志强, 王超, 鄢雪龙, 2014. 壳幔幔岩浆混合作用与陆内环境高Sr/Y斑岩的形成及成矿: 实例与探讨. 岩石学报, 2014, 30: 2020-2030.
[24]陈长健, 陈斌*, 王志强, 2017. 宁芜地区中生代富钾和富钠火山岩的源区特征：岩石学和地球化学证据. 岩石学报, 33: 415-439.
total24 3/3
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