佛罗里达州立大学范文渊助理教授学术报告

地球系统科学论坛第672期：范文渊助理教授学术报告会

应遊雅堂 競馬王墩教授邀请，佛罗里达州立大学范文渊助理教授来校交流并做学术报告。

报告时间：2019年6月21日（周五）上午10：30

报告地点：地质斋（主楼308）

报告题目：Physics of seismic sources revealed by advanced array analyses

报告人简介：Wenyuan Fan is an assistant Professor of Geophysics at Florida State University.In 2008 and 2011, he received his bachelor's and master's degrees from the Department of Geophysics, Peking University, and his Ph.D. in geophysics from the University of California, San Diego in 2017. Postdoctoral research at the Woods Hole Oceanographic Institution from 2018 to 2019. In 2019, he was appointed assistant professor of geophysics at Florida State University. The main research direction: Array Seismology. Research interests: marine geophysics, earthquake source kinematic and dynamic processes, earthquake interaction and triggering, waveform modeling, environmental seismology, and ocean and solid earth interaction. He has received the James Postdoctoral Research Funds, 2017 China Scholarship Council Award, Woods Hole oceanographic Institution Postdoctoral Scholarship, lamont-Doherty Earth Observatory Postdoctoral Fellowship (declined), AGU Outstanding Student Paper Award, Graduate Student Fellowship at Peking, etc. . He has published many academic papers in journals such as Geophysical Research Letters, Tectono-physics, Science, Seismol, etc. Currently, h-index: 10 (Web of Science), 11 (Google Scholar). A total of 368 citations were cited, with average of 19.37 citations per article (Science Citation Index as of 02/19/2019). He is currently a referee for journals such as Geophysical Research Letters, Geophysical Journal International, Bulletin of the Seismological Society of America, Journal of Geophysical Research:,Solid Earth, Tectonophysics, Pure and Applied Geophysics, Journal of Seismology. Personal webpage: http://myweb.fsu.edu/wfan/

报告内容简介：Large seismic arrays have provided platforms for developments of earthquake source imaging techniques. Results from these data and techniques have improved our understandings of earthquake rupture propagations. For example, back-projection source models show that large earthquakes (M > 7) often rupture multiple faults and may contain a number of large subevents. The fault systems hosting these earthquakes are mostly in plate-boundary regions and they often interact with each other. In addition, small earthquake rupture dynamics can be resolved at great precision with the Large-N nodal arrays, suggesting future research directions. Moreover, abnormal slip events, including glacier quakes and landslides, can be detected with array analysis, which are missed by most of the standard catalogs because of their deficiencies in high frequency. These findings have demonstrated the power of large dataset, and have advanced our understandings of earthquake physics. We will discuss complex earthquake kinematics observed in a wide range of slip events from dense array analyses.

欢迎大家参加！

遊雅堂 競馬

GPMR国家重点实验室

2019年6月