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牛耀龄1,2,3, 龚红梅1,2, 王晓红1,2, 肖媛媛1,2, 郭鹏远1,2, 邵凤丽1,2,4, 孙普1,2,4, 陈硕1,2,4, 段梦1,2,5, 孔娟娟1,2,4, 王国栋1,2, 薛琦琪1,2,5, 高雅洁1,2,4, 洪迪1,2,4

Some Key Problems on the Petrogenesis of Seafloor Basalts, Abyssal Peridotites and Geodynamics—A Non-traditional Isotope Approach
Niu Yaoling1,2,3, Gong Hongmei1,2, Wang Xiaohong1,2, Xiao Yuanyuan1,2, Guo Pengyuan1,2, Shao Fengli1,2,4, Sun Pu1,2,4, Chen Shuo1,2,4, Duan Meng1,2,5, Kong Juanjuan1,2,4, Wang Guodong1,2, Xue Qiqi1,2,5, Gao Yajie1,2,4, Hong Di1,2,4
玄武岩浆演化过程中随Mg#减小,全岩Fe,Fe3+/∑Fe, f O2与δ57Fe的协变关系(简化自参考文献[52]) 绿色方块数据来自参考文献[49],金黄色圆圈数据来自参考文献[52]