The seismicity in the middle section of the Altyn Tagh Fault system revealed by a dense nodal seismic arrayOA
The left-lateral Altyn Tagh Fault(ATF) system is the northern boundary of the Qinghai-Xizang Plateau, separating the Tarim Basin and the Qaidam Basin. The middle section of ATF has not recorded any large earthquakes since1598…查看全部>>
Shi Yao;Tao Xu;Yingquan Sang;Lingling Ye;Tingwei Yang;Chenglong Wu;Minghui Zhang
Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China University of Chinese Academy of Sciences,Beijing,100049,ChinaKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China Department of Earth and Space Sciences,Southern University of Science and Technology,Shenzhen,518055,ChinaKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China Department of Earth and Space Sciences,Southern University of Science and Technology,Shenzhen,518055,China University of Chinese Academy of Sciences,Beijing,100049,ChinaDepartment of Earth and Space Sciences,Southern University of Science and Technology,Shenzhen,518055,ChinaKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China University of Chinese Academy of Sciences,Beijing,100049,ChinaKey Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,100029,China Innovation Academy for Earth Science,Chinese Academy of Sciences,Beijing,100029,ChinaSchool of Information Engineering,Shandong University of Aeronautics,Binzhou,256603,China
地球科学
Altyn Tagh FaultMachine learningSeismicityDense seismic array
《Earthquake Research Advances》 2024 (3)
P.7-15,9
supported by the Second Tibetan Plateau Scientific Expedition and Research Program (STEP, 2019QZKK0701-02)the National Natural Science Foundation of China (Grant 42104102 and 42130807)。
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