S31F:
Next-Generation Seismic Source Studies Posters
Submit an Abstract to this Session
Session ID#: 44291
Session Description:
Seismic source studies are fundamental to seismology. Recently, correlation-based detection and location methods have dramatically improved seismic monitoring capability. For other aspects of source studies, machine learning shows promise in tasks such as phase picking and association, event detection, event location, and event classification. Correlation-based double-difference location methods can vastly improve the precision of earthquake location. Polarity, phase amplitude, S/P amplitude ratio, and full waveform techniques have led to great improvements in focal mechanism determination and reliability. There have also been important improvements in source models spanning point source to full finite-fault models. Despite this progress, opportunities remain for improvements in seismic monitoring ability, including seismic monitoring in real time, and in streamlining the components of source characterization into a seamless workflow. This session aims to highlight new methods and applications in detection, location and characterization of seismic events in different aspects of seismological studies.
Primary Convener: Miao Zhang, Stanford University, Stanford, CA, United States
Conveners: David R Shelly, US Geological Survey, Menlo Park, CA, United States, Francesco Grigoli, ETH Zurich, Swiss Seismological Service, Zurich, Switzerland and Kazutoshi Imanishi, Geological Survey of Japan, AIST, Tsukuba, Japan
Primary Liaison: Miao Zhang, Stanford University, Stanford, CA, United States
Chairs: Miao Zhang, Dalhousie University, Department of Earth and Environmental Sciences, Halifax, NS, Canada, David R Shelly, U.S. Geological Survey, Geologic Hazards Science Center, Golden, United States, Francesco Grigoli, University of Potsdam, Potsdam, Germany and Kazutoshi Imanishi, Geological Survey of Japan, AIST, Tsukuba, Japan
OSPA Liaison: Miao Zhang, Dalhousie University, Department of Earth and Environmental Sciences, Halifax, NS, Canada
Abstracts Submitted to this Session:
Pawan Bharadwaj1, Yusuke Mukuhira2, Laurent Demanet3, Michael Fehler4 and Aimé Fournier4, (1)Massachusetts Institute of Technology, Earth Resources, Cambridge, MA, United States, (2)Tohoku University, Institute of Fluid Science, Sendai, Japan, (3)Massachusetts Institute of Technology, Cambridge, United States, (4)Massachusetts Institute of Technology, Cambridge, MA, United States
Francesco Grigoli1, Luca Scarabello1, Maren Boese2, Bernd Weber3, Stefan Wiemer1 and John F Clinton4, (1)ETH Zurich, Swiss Seismological Service, Zurich, Switzerland, (2)ETH Zurich, Department of Earth Sciences, Institute of Geophysics, Zurich, Switzerland, (3)gempa GmbH, Potsdam, Germany, (4)ETH Swiss Federal Institute of Technology Zurich, Swiss Seismological Service (SED), Zurich, Switzerland
Fengzhou Tan, University of Victoria, School of Earth and Ocean Sciences, Victoria, BC, Canada, Honn Kao, Geological Survey of Canada, Pacific Geoscience Centre, Sidney, BC, Canada, Edwin Nissen, University of Victoria, Dept. of Earth and Ocean Sciences, Victoria, BC, Canada and David W S Eaton, University of Calgary, Department of Earth, Energy, and Environment, Calgary, AB, Canada
Ana C Aguiar, Lawrence Livermore National Laboratory, Livermore, United States and Stephen C Myers, Lawrence Livermore Natl Lab, Livermore, CA, United States
Min Liu, China University of Geosciences (Beijing), Beijing, China and Hongyi Li, China University of Geosciences (Beijing), School of Geophysics and Information Technology, Beijing, China
Kazutoshi Imanishi and Takahiko Uchide, National Institute of Advanced Industrial Science and Technology (AIST), Geological Survey of Japan, Tsukuba, Japan
Keith lynn McLaughlin, Organization Not Listed, Washington, VA, United States and David H Salzberg, Leidos, San Diego, CA, United States
Jannes Kinscher1, Kadek Hendrawan Palgunadi2, Natalia Poiata3, Francesca De Santis1, Pascal Bernard4 and Emmanuelle Klein1, (1)INERIS Institut National de l’Environnement Industriel et des Risques, Nancy, France, (2)King Abdullah University of Science and Technology, Thuwal, Saudi Arabia, Thuwal, Saudi Arabia, (3)National Institute for Earth Physics, Ilfov, Romania, (4)Institut de Physique du Globe de Paris (IPGP), Université Paris Cité, Paris, France
Oluwaseun Idowu Fadugba, University of Memphis, Center for Earthquake Research and Information (CERI), Memphis, TN, United States, Charles A Langston, University of Memphis, Center for Earthquake Research and Information, Memphis, United States and Christine Ann Powell, University of Memphis, Memphis, TN, United States
Han Li, Hohai University, College of Oceanography, Nanjing, China, Xu Chang, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China and ZhenXing Yao, Institute of Geology and Geophysics, Chinese Academy of Sciences, Key Laboratory of Earth and Planetary Physics, Beijing, China
Xu Chang, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, Han Li, Hohai University, College of Oceanography, Nanjing, China and Hongyu Zhai, Institute of Geology and Geophysics, Chinese Academy of Sciences, Key Laboratory of Shale Gas and Geoengineering, Beijing, China
Saulė Simutė, ETH Zurich, Department of Earth Sciences, Institute of Geophysics, Zurich, Switzerland and Andreas Fichtner, ETH Zurich, Institute of Geophysics, Zurich, Switzerland
Wenze Deng, CENC China Earthquake Networks Center, Beijing, China, Jinlai Hao, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, Lei Zhang, Tsinghua University, Beijing, China and Chen Ji, University of California Santa Barbara, Santa Barbara, CA, United States
JinLai Hao, IGG, Chinese Academy of Sciences, Beijing, China, Lei Zhang, Tsinghua University, Beijing, China, Wenze Deng, CENC China Earthquake Networks Center, Beijing, China, Chen Ji, University of California Santa Barbara, Santa Barbara, CA, United States and ZhenXing Yao, Institute of Geology and Geophysics CAS, Beijing, China
Miao Zhang1, William L Ellsworth2, Gregory C Beroza2, Felix Waldhauser3, Lauro Chiaraluce4, Maddalena Michele4 and Margarita Segou5, (1)Dalhousie University, Department of Earth and Environmental Sciences, Halifax, NS, Canada, (2)Stanford University, Department of Geophysics, Stanford, CA, United States, (3)Columbia University, Lamont-Doherty Earth Observatory, Palisades, United States, (4)Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy, (5)British Geological Survey, Edinburgh, United Kingdom
David Paul Schaff1, Won-Young Kim1, Paul G Richards2, Eunyoung Jo3 and Yonggyu Ryoo3, (1)Lamont-Doherty Earth Observatory, Palisades, NY, United States, (2)Columbia University, Palisades, NY, United States, (3)Korea Meteorological Administration, Seoul, South Korea
Jieyuan Ning, Peking University, School of Earth and Space Sciences, Beijing, China
Xiaohan Chen, University of Science and Technology of China, Hefei, China and Lianxing Wen, Stony Brook University, Department of Geosciences, Stony Brook, United States
Yingjie Xia1, Sidao Ni2 and Xiaofei Chen1, (1)Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, China, (2)Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan, China
Qiaoxia Liu1, Sidao Ni2, Yong Qiu1 and Ming Zhou1, (1)Geophysical Exploration Center, China Earthquake Administration, Zhengzhou, China, (2)Innovation Academy for Precision Measurement Science and Technology, Chinese Academy of Sciences, Wuhan, China