JpGU-AGU Joint Meeting 2017

Presentation information

[EE] Oral

S (Solid Earth Sciences) » S-SS Seismology

[S-SS05] [EE] earthquake statistics, physics-based earthquake forecasting, and earthquake model testing

Wed. May 24, 2017 1:45 PM - 3:15 PM A05 (Tokyo Bay Makuhari Hall)

convener:Danijel Schorlemmer(GFZ German Research Centre for Geosciences), Naoshi Hirata(Earthquake Research Institute, the University of Tokyo), Matt Gerstenberger(GNS Science), Hiroshi Tsuruoka(Earthquake Research Institute, Tokyo Univ.), Jiancang Zhuang(Institute of Statistical Mathematics), Chairperson:Hiroshi Tsuruoka(Earthquake Research Institute, Tokyo Univ.), Chairperson:Kazuyoshi Nanjyo(University of Shizuoka)

3:00 PM - 3:15 PM

[SSS05-06] An extensive study of clustering features of seismicity in Italy during 2005 to 2016

*Jiancang Zhuang1,4, Yicun Guo2, Maura Murru3, Giuseppe Falcone3, Matteo Taroni3, Rodolfo Console3 (1.Institute of Statistical Mathematics, 2.Earthquake Research Institute, University of Tokyo, 3.Istituto Nazionale di Geofisica e Vulcanologia, 4.the Graduate University for Advanced Studies)

Keywords:Earthquakes in Italy , space-time modelling

Compiled by INGV, the ISIDE catalog includes high quality records of the occurrence times, locations, and magnitude of earthquakes that occurred in the Italy region since 2005-4-16. To study the characteristics of seismicity in Italy, we use the space-time ETAS model and several extended forms. Our results show:
Seismicity clustering features are quite different from region to region. According to the ETAS parameters, the whole study region can be divided into four subregions.
The rupture geometries of large earthquakes, including the 2009-4-6 M6.3 L'Aquila, the 2012-5-20 M6.1 Emilia, the 2016-0-24 M6.0 Amatrice, the 2016-10-30 M6.2 Norcia earthquakes, control the spatial locations of their direct aftershocks. These direct aftershock aftershock mainly concentrate near, some parts close to the parts on the rupture plane with large slips but seldom overlap with them, indicating that aftershocks are the continuation of the rupture process of the mainshocks.
When the focal depth is considered in seismicity modeling, improved probability forecasting of seismicity and hazard assessment can be obtained.