机译:前里山组合岩体(华南)富氟高分异花岗岩的成因及对多金属矿化的启示
School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, Anhui, China,Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871, China;
Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871, China;
Key Laboratory of Orogenic Belts and Crustal Evolution, Peking University, Beijing 100871, China;
Fluorine-rich; Highly differentiated granites; Melt-rock/fluid interaction; A-type granite;
机译:高度分化的富含氟,碱性花岗岩岩浆与稀有金属矿化联系起来:以南天山地区的Boziguo'er稀有金属花岗岩,新疆,中国
机译:华南南岭晚中生代前山山A(2)型花岗岩的产生:对石竹园钨锡矿化及构造演化的启示
机译:黄沙坪多金属矿床(中国湖南南部)A型花岗岩的地球化学:对花岗岩演化和相关矿化的意义
机译:华南中部地区燕山早期花岗岩的多阶段成矿作用:稀土地球化学的意义
机译:内华达山脉南部的沉积物垂体的非模态部分熔融及其对岩浆内同位素异质性深层成因的启示。
机译:中国南方重稀土矿化成因
机译:华南南岭晚中生代千里山A(2)型花岗岩的产生:对石竹园钨锡矿化及构造演化的启示