机译:南合里山断裂带(中国西北河西走廊)的第四纪晚期滑移速率及其对青藏高原东北向生长的影响
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China,Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China;
Department of Geological Sciences, and Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado 80309, USA;
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China;
Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China;
Institute of Geology Chinese Academy of Geological Sciences, Beijing 100037, China;
机译:河西走廊(中国祁连山北部)逆冲断层的晚第四纪滑动速率及其对青藏高原东北向发育的影响
机译:河西走廊(中国祁连山北部)逆冲断层的晚期第四纪滑动速率及其对青藏高原东北向发育的影响
机译:沿着河西走廊及其南戈山南戈山南方的北季度罢工滑倒及其构造影响
机译:东北藏高原南海山故障的垂直位移分布从高分辨率地形数据得出
机译:中国西北阿尔金断裂带中部的最新第四纪滑动历史,来自断层阶地立管。