机译:华北克拉通晚中生代房山低镁埃达克质岩体的镁铁质岩脉和高镁埃达克质岩群的成岩作用
State Key Laboratory of Geological Processes and Mineral Resources, China University of Ceosciences, Wuhan 430074, China,Faculty of Earth Sciences, China University of Ceosciences, Wuhan 430074, China;
Editorial Office of Journal, China University of Geoscience, Wuhan 430074, China;
State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China;
State Key Laboratory of Geological Processes and Mineral Resources, China University of Ceosciences, Wuhan 430074, China,Faculty of Earth Sciences, China University of Ceosciences, Wuhan 430074, China;
Faculty of Earth Sciences, China University of Ceosciences, Wuhan 430074, China;
high-mg adakitic enclave; low-mg adakitic host; mafic dyke; magma mixing; North China Craton;
机译:沿北北方南部最南端的早期白垩纪低Mg adaAkitic岩石的浮动性:对中生代地壳演进的影响
机译:中国西北地区北部祁连造山带早古生代低镁和高镁埃达克质岩石的成因:从地壳增厚过渡到伸展变薄的意义
机译:由部分结晶形成的同碰撞阿达克质花岗岩-来自青藏高原北缘北祁连造山带曲木山岩体中封闭的镁铁质岩浆飞地(MME)的见解
机译:硅质熔融橄榄岩的相互作用:对华北克拉通中生代高镁闪长岩的成岩作用和岩石圈演化的制约
机译:上地壳岩浆管道系统的演变:中国北京的白垩纪房山岩体,美国中生代中塞拉弧和美国亚利桑那州中新世银河破火山口的地质,岩石学,地球化学和结构记录的比较。