Conference Program - 4thicce.com

1 International Conferencefor the Decade Memoryof the Wenchuan EarthquakewithThe 4th International Conferenceon Continental Earthquakes(The 4th icce )andThe 12th General Assembly ofthe Asian SeismologicalCommission (ASC)May 12-14 2018 Chengdu Sichuan ChinaConference 12 2018 5 12-14 Organized and hosted byMinistry of Emergency Management of the People's Republic of ChinaPeople's Government of Sichuan ProvinceChina earthquake Administration0809 Crystal BallroomCrystal Ballroom( II )Crystal Ballroom( III )Jinjiang HallQingyang HallChenghua HallShujin HallShuhan HallShushan HallShushui HallShuyun HallShufeng HallTianfu HallShudu HallXindu HallLevel 5 Level 5 Level 5 Level 5 Level 5 Level 5 Level 3 Level 3 Level 3 Level 3 Level 3 Level 3 Level 3 Level 3 Level 5 Fri, May 11, 18:30-20:00 Ice BreakerSat, May 12, 08:30-10:00 POC 09:00-10:00 Sat, May 12, 10:30-12:00PK-1SP-1 Sat, May 12, 12:00-13:30 LunchBM-2 Sat, May 12, 13:30-15:00S3-3-6S1-1-3S1-2-3 ASC SOCTK-2S3-1-5S2-1-17 TCEAGND SOCTK-1S1-2-2S2-1-3 China RE SOCS4-1-2 Sat, May 12, 15:30-18:00S3-3-6S1-1-2S1-2-3TK-2S2-2-3S 3-1-5S2-1-1TK-1S3-1-3S1-2-2S2-1-3S4-1-2 Sun, May 13, 08:30-10.

2 00S1-2-3S3-1-6S2-4-1S2-4-2TK-3S3-1-3S2-3 -4BM-5S1-1-1S3-1-1SP-2 Sun, May 13, 10:30-12:00PK-2 Sun, May 13, 12:00-13:30 LunchBM-6 LunchBM-3 Sun, May 13, 13:30-15:00S2-3-2S2-2-1S3-1-6S2-4-1TK-4S 4-1-4S3-1-3S2-3-4S4-1-3S1-2-4TK-5S3-1-1 Sun, May 13, 15:30-18:00S2-2-1S2-3-6S2-4-1S2-2-2S3-1- 3S2-3-4S4-1-3S1-2-4S3-1-1 Mon, May 14, 08:30-10:00BM-7S2-2-1S2-1-2S4-2-1S1-2-1T K-6S3-1-3S2-3-4S4-1-1S2-3-5S3-1-7SP-3 Mon, May 14, 10:30-12:00PK-3 Mon, May 14, 12:00-13:30 LunchBM-4 Mon, May 14, 13:30-15:00S5-1-2S2-2-1S2-1-2S2-5-3S1-2- 1S3-1-3S2-4-3S5-1-1S2-3-1S3-2-4 Mon, May 14, 15:30-17:00S5-1-2S2-2-1S2-1-2S2-5-3S1-2- 1S3-1-3S2-4-3BM-1S2-3-1S3-2-4 Mon, May 14, 17:10-18:00 PCCPK: Plenary Keynote; TK: Thematic Keynote; POC: Plenary Opening Ceremony; SOC: Session Opening Ceremony; PCC: Plenary Closing Ceremony.

3 BM: Business MeetingSP-1: Poster Session, including S1-1-2 P, S1-1-3 P, S1-2-2 P, S1-2-3 P, S2-1-1 P, S2-1-3 P, S2-2-3 P, S3-1-3 P, S3-1-5 P, S3-3-6 P, S4-1-2 PSP-2: Poster Session, including S1-1-1 P, S1-2-3 P, S1-2-4 P, S2-2-1 P, S2-2-2 P, S2-3-2 P, S2-3-4 P, S2-3-6 P, S2-4-1 P, S2-4-2 P, S3-1-1 P, S3-1-3 P, S3-1-6 P, S4-1-3 P, S4-1-4 PSP-3: Poster Session, including S1-2-1 P, S2-1-2 P, S2-2-1 P, S2-3-1 P, S2-3-4 P, S2-3-5 P, S2-4-3 P, S2-5-3 P, S3-1-3 P, S3-1-7 P, S3-2-4 P, S4-1-1 P, S4-2-1 P, S5-1-1 P, S5-1-2 PProgram at a glance1011 Keynote Iectures1213 Saturday, 12 MayPlenary Keynote 1 Time: 10:30-12:00 Venue: Crystal Ballroom (Level 5)Convenor: Yun-tai CHEN, Alexey ZAVYALOV 10:30-11:00 Guoguang ZHENG Decade review and prospective of seismic risk mitigation in China11:00-11:30 Paul TAPPONNIER DEM modelling of the Tertiary Deformation of the Pamir and adjacent blocks 11:30-12:00 Invited Lecture by Sichuan Provincial GovernmentSunday, 13 MayPlenary Keynote 2 Time: 10:30-12:00 Venue: Crystal Ballroom I (Level 5)Convenor: Yong CHEN, Giuliano PANZA10:30-11:00 John E.

4 VIDALE SCEC and the science of earthquake forecasts11:00-11:30 Yun-tai CHEN Fast inversion of earthquake rupture process and its application in earthquake emergency responses11:30-12:00 Ikuo TOWHATA Disaster-proneness of residential land and efforts towards improvementMonday, 14 MayPlenary Keynote 3 Time: 10:30-12:00 Venue: Crystal Ballroom I (Level 5)Convenor: Zhongliang WU, Paramesh BANERJEE 10:30-11:00 Peizhen ZHANG Seismogenis structure and mechanism of the 2008 Wenchuan earthquake , Sichuan, China 11:00-11:30 Thorne LAY The 2008 Wenchuan earthquake and advances in earthquake science11:30-12:00 Jeffrey FREYMUELLER The earthquake cycle on the Denali fault, Alaska, and its implications for the study of great earthquakes in Asia1415 The 2008 Wenchuan earthquake and the Practice in China for earthquake Disaster ResilienceGuoguang ZHENGVice-Minister Ministry of Emergency Management People's Republic of China Administrator, China earthquake AdministrationSaturday, 12 May From 10:30-11.

5 00 Crystal Ballroom (Level 5)1617 DEM modelling of the Tertiary Deformation of the Pamir and adjacent blocksPaul TAPPONNIERN anyang Technological UniversityMember of the French Academy of Sciences, Foreign associate member of the National Academy of Science (USA),Fellow of American Geophysical UnionSaturday, 12 MayFrom 11:00-11:30 Crystal Ballroom (Level 5)The occurrence of two recent, shallow, strike-slip earthquakes in the Pamirs help elucidate the tectonic processes that control 3D crustal deformation around the Northwest corner of the India/Asia collision zone. InSAR data, and the focal mechanisms of these two events - 12/2015, MW , South-Karakul, and 11/2016, MW , West-Muji earthquakes are consistent with respectively left- and right-lateral strike-slip motion on two conjugate, respectively NE- and EW-striking faults.

6 On high-resolution optical images, the two corresponding active fault- systems can be mapped for several hundreds kilometres to connect with the Pandchir/Chaman and Karakorum fault systems, respectively. The former - hitherto undocumented - connection across high-mountain terrane and glacial topography, is marked by clear surface-breaks and alignments of large, river-damming landslides. DEM modelling of the Tertiary Deformation of the Pamir and adjacent blocksPaul Tapponnier, Jiao Liqing, Priyamvada Nanjundiah, and Sylvain BarbotEOS/ASE, Nanyang Technological University, SingaporeThe two fault systems accommodate part of India/Tibet s northwest prong s convergence, as it crashes on the strong, southern edge of Paleozoic Asia.

7 They foster westward and eastward extrusion of Tajikistan and Tibet, respectively. Key elements of such complex, large-scale faulting and continental strain may be modelled using the Yade DEM deformation and the science of earthquake forecastsJohn E. VIDALES outhern California earthquake Center, DirectorSunday, 13 MayFrom 10:30-11:00 Crystal Ballroom I (Level 5)This talk reviews new ideas about earthquakes that we ve learned at the Southern California earthquake Center (SCEC), and where we re headed danger and cost of earthquakes has focused public fear and research effort in California since long before the devastating 1906 San Francisco and 1933 Long Beach events.

8 Precise earthquake prediction, heralded as imminent in the 1970s, has faltered, maybe permanently, but nevertheless there is at USC, with 16 core institutions and more than 60 affiliated organizations, SCEC involves more than 1000 quake cognoscenti. Funding comes from the National Science Foundation, the United States Geological Survey, and special projects with foundation and corporate partners. We are uncloaking the mysteries in plate tectonics, the San Andreas fault system, and how the ground is driven to shake. SCEC investigates all aspects of earthquakes from theoretical models through detailed observations to hazard maps. We foster collaboration among the fields of science and engineering research, computer science, communication and outreach to develop integrated research products used by various central point of this intense research, and the result that most directly benefits those living in California, is the improvement of maps of earthquake danger.

9 We find the tectonic fault lines, gauge their geological rates of motion, and model their patterns of rupture and reloading in order to resolve the earthquakes we are likely to face. Bysimulating, in the nation s largest computers, the trembling for millions of those earthquakes through high-fidelity models of the rocks just under our feet, we are step-by-step wringing the uncertainty out of the nation s earthquake hazard are on the verge of making the hazard estimation process entirely physics-based - built on models with realistic patterns of fault slip on realistic fault surfaces, accurate models of geological structure, and with the latest models of earthquake cycles on fault systems.

10 Some aspects of the old hazard maps are confirmed. Other aspects, particularly the strength of the reverberations in the soft Los Angeles basin and its basin brothers across the state, may have been underestimated. A few places are now assessed as safer than before, but answers are not yet is allowing more apt emergency preparations and building and retrofitting laws, and in the process giving us a deeper understanding of the physics of earthquakes and the geological evolution of the Southern California natural and the science of earthquake forecastsJohn E. Vidale, Greg C. Beroza, Thomas H. JordanUniversity of Southern California2021 Fast inversion of earthquake rupture process and its application in earthquake emergency responsesYun-tai CHENU niversity of Chinese Academy of SciencesAcademician of the Chinese Academy of SciencesSunday, 13 MayFrom 11:00-11:30 Crystal Ballroom I (Level 5)Fast inversion of earthquake rupture process and its application in earthquake emergency responsesChen Yun-tai1,2, Zhang Yong1, Xu Li-Sheng21.