supported by the National Natural Science Foundation of China (No. 41974109);the Equipment Development Project of CAS (No. YJKYYQ20190075);grants of the Wong K. C. Education Foundation (No. GJTD-201904);CAS ‘The Belt and Road’ Master Fellowship Program。
An attempt has been made to reveal the upper mantle velocity structure of the eastern Tibetan Plateau using 628 teleseismic events recorded from 2003 to 2009 at 95 stations.A total of 8 532 Pwave arrival time residual...
supported by funding from the Strategic Priority Research Program(B)of Chinese Academy of Sciences through grant XDB18010304;Natural Science Foundation of China through grant 41322027,41374060,41374079,41661164035
P-wave waveforms in the distance range between 12°and 30°were analyzed to investigate upper-mantle P velocity structures beneath the Tibetan Plateau and surrounding areas.The waveform data from 504 earthquakes with ...
supported by the National Natural Science Foundation of China (No. 40730317), and China Scholarship Council
Seismic studies of the crustal structure beneath the Three Gorges Reservoir(TGR) region in Central China have been limited by the sparse and uneven distribution of seismic stations.To in-crease the station coverage,...
Supported by the National Natural Science Foundation of China under Grant Nos 40473034, 40404007, 10574055 and 50532020, and the National Basic Research Programme of China under Grant No 2005CB724404.
The electrical conductivity of molten olivine is studied up to 3720K and 13.2 GPa. The results indicate that the electrical conductivity of molten olivine exhibits the perfect Arrhenius behaviour. The activation energ...
Supported by the National Natural Science Foundation of China (Grant Nos.40242014;49832030) and Peking University (Project 985)
The microstructures of the mantle tectonites in the Zunhua Neoarchean ophiolitic melange are mainly coarse-mosaicstructures with locally interstitial impregnated melts. Olivine and orthopyroxene occur as residual porp...