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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
Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China|Chinese Acad Geol Sci, Inst Geol, State Key Lab Continental Tecton & Dynam, Beijing 100037, Peoples R China|Kunming Univ Sci & Technol, Fac Land Resource Engn, Kunming 650093, Peoples R China;
Chinese Acad Geol Sci, Inst Geol, State Key Lab Continental Tecton & Dynam, Beijing 100037, Peoples R China;
Chinese Acad Geol Sci, Inst Geol, State Key Lab Continental Tecton & Dynam, Beijing 100037, Peoples R China;
Jilin Univ, Coll Earth Sci, Changchun 130061, Peoples R China;
China Geol Survey, Nanjing Ctr, Nanjing 210016, Jiangsu, Peoples R China;
China Geol Survey, Chengdu Ctr, Chengdu 610081, Peoples R China;
Chinese Acad Geol Sci, Inst Geol, State Key Lab Continental Tecton & Dynam, Beijing 100037, Peoples R China;
Low-Mg adakitic rocks; High-Mg adakitic rocks; North Qilian orogenic belt; Crustal thickening; Delamination;
机译:NW中国北祁连和北阿尔伦orenatenic腰带的连续性:来自新发现的猴古代低mg和高镁adakitic岩石的证据
机译:早古生代白银火山岩的地球化学(对北祁连造山带构造演化的启示)
机译:中国西北青藏高原北缘泥盆纪与造山运动有关的火山沉积岩:对北柴达木造山带古生代构造过渡的启示
机译:中国西部祁连造山带鱼石沟蛇纹岩铬铁矿成矿作用的地球化学约束
机译:中国中央造山带硅质岩的分布微结构和地球化学特征:对热液沉降模型的启示
机译:早古生代白银火山岩地球化学特征:北祁连造山带构造演化的意义