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机译:东昆仑造山带220 Ma之前的地壳增厚:从小诺木洪岩体的晚三叠世花岗质体中获得的见解
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China,Gold Geological Institute of CAPF, Langfang 065000, China;
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, No. 29, Xueyuan Road, Beijing 100083, China;
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China;
School of Earth and Environmental Sciences, James Cook University, Townsville 4811, Queensland, Australia;
Gold Geological Institute of CAPF, Langfang 065000, China;
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China,Gold Geological Institute of CAPF, Langfang 065000, China;
Geochronology; Geochemistry; Adakite; Mafic microgranular enclave; Paleo-Tethys; East Kunlun;
机译:改造旧大陆岩石圈:造山带地壳演化的重要机制,青藏高原北部东昆仑造山带的三叠世I型花岗岩类证明了这一点
机译:来自中国东昆仑造山带的三叠纪花岗岩的瘀细胞,NW中国:对大陆地壳增长的影响与碰撞后环境
机译:青藏高原北部东昆仑造山带花岗岩类岩石成因的地球化学约束:通过共碰撞长英质岩浆作用对大陆壳生长的影响
机译:矽卡岩体系中的Nb / Ta分离:东昆仑造山带白石崖铁矿床磁铁矿的原位织构和化学分析的证据
机译:碰撞后背景下花岗岩成岩过程中的地幔-壳相互作用:罗马尼亚南部喀尔巴阡山脉的达努比人瓦里斯坎岩体的见解