The Crustal-scale Shortening on the Eastern Margin of the Tibet Plateau: the Main Mechanism of Uplift-Revealed from Deep Seismic Reflection Profiles Across the Min Shan and Hu Ya Faults
School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou, China Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou, China
School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou, China
Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
SinoProbe Center, Chinese Academy of Geological Sciences, Beijing, China
Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
School of Earth Sciences and Engineering, Sun Yat-Sen University, Guangzhou, China
Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China
Chinese Academy of Geological Sciences, Beijing, China