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Velocity structure of layered block and deep dynamic process in the lithosphere beneath the Yinshan orogenic belt and Ordos Basin
The Yinshan orogenic Belt in the northern margin of Ordos Basin is not only a transition region between strong and weak tectonic activities, but also a basin/mountain coupling zone, so there are… Expand
A STUDY OF DEEP SEISMOGENIC ENVIRONMENT IN LUSHAN MS7.0 EARTHQUAKE ZONE BY WIDE‐ANGLE SEISMIC REFLECTION/REFRACTION PROFILE
After the Lushan earthquake in April, 2013, the Lushan earthquake scientific investigations headquarter was quickly established by China Earthquake Administration to investigate the deep structure… Expand
Effects of shading on photosynthesis, and other physiological and biochemical characteristics in tree peony.
Structure of the seismic wave property and lithology deduction of the upper crust beneath the Yinshan orogenic belt and the northern Ordos block
Review of the Application of Machine Learning in Seismic Detection and Phase Identification
Crustal Low Velocity Zone Beneath The Northeastern Tibetan Plateau
The young and growing northeastern Tibetan plateau is an ideal region for studying the uplift and outward growth of Tibetan Plateau. Moreover, the northeastern margin is significant important to… Expand
Upper crust structure of eastern A'nyemaqên suture zone: Results of Barkam-Luqu-Gulang deep seismic sounding profile
Barkam-Luqu-Gulang deep seismic sounding profile runs from north of Sichuan Province to south of Gansu Province. It is located at the northeastern edge of Tibetan Plateau and crosses eastern… Expand