机译:临夏盆地晚新生代河流湖相磁化率增加及其对青藏高原隆升的影响
MOE, Key Laboratory of Western China's Environmental Systems, Collaborative Innovation Centre for Arid Environments and Climate Change,Lanzhou University, Lanzhou 730000, China;
Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Institute, Chinese Academy of Sciences,Donggang West Road 320#, Lanzhou 730000, China;
Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;
Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;
School of Earth Sciences & Key Laboratory of Western China's Mineral Resources of Gansu Province, Lanzhou University, Lanzhou 730000, China;
机译:昆仑Pass陷盆地晚新生代高分辨率地层学及其对青藏高原北部隆升的启示
机译:昆仑Pass陷盆地晚新生代高分辨率地层学及其对青藏高原北部隆升的启示
机译:柴达木盆地西部新生代矿床的磁性地层学及其对青藏高原东北缘地表隆升的意义
机译:随着修改的上升:化石鱼目睹了他们自己的集团在新生代晚期的西藏高原隆起的适应
机译:在新生代藏高原藏边缘的构造与气候之间的相互作用:西藏高原和西北地区西北地区的案例研究促进了自新世纪以来中纬度亚洲