Lithospheric Structure Beneath the NE Iranian Plateau Revealed by S-wave Receiver Function Migration
Zimu Wu1,2, Ling Chen1,3, Morteza Talebian4, Xu WANG2,5, Mingming Jiang3,6, Yinshuang Ai7, Mohammad Mahdi Khatib8, Yumei He3,9, Xiaofeng Liang10 and Liang Zhao1,11, (1)State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, (2)University of Chinese Academy of Sciences, College of Earth Sciences, Beijing, China, (3)CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing, China, (4)Research Institute for Earth Sciences, Geological Survey of Iran, Tehran, Iran, (5)Institute of Geology and Geophysics, CAS, Beijing, China, (6)Key Laboratory of Planetary Science and Frontier Technology, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, (7)Institute of Geology and Geophysics, Chinese Academy of Sciences, Key Laboratory of Planetary Science and Frontier Technology, Beijing, China, (8)University of Birjand, Department of Geology, Birjand, Iran, (9)Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, (10)Institute of Geology and Geophysics, Chinese Academy of Sciences, State Key Laboratory of Lithospheric Evolution, Beijing, China, (11)Institute of Geology and Geophysics, Chinese Academy of Sciences, Key Laboratory of Deep Petroleum Intelligent Exploration and Development, Beijing, China
