日本地球惑星科学連合2022年大会

講演情報

[E] 口頭発表

セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS04] Seismic Spectra for Source, Subsurface Structure, and Strong-motion Studies

2022年5月23日(月) 09:00 〜 10:30 103 (幕張メッセ国際会議場)

コンビーナ:内出 崇彦(産業技術総合研究所 地質調査総合センター 活断層・火山研究部門)、コンビーナ:Abercrombie Rachel E(Boston University)、Ma Kuo-Fong(Institute of Geophysics, National Central University, Taiwan, ROC)、コンビーナ:染井 一寛(一般財団法人地域地盤環境研究所)、座長:内出 崇彦(産業技術総合研究所 地質調査総合センター 活断層・火山研究部門)、Rachel E Abercrombie(Boston University)、Ma Kuo-Fong(Institute of Geophysics, National Central University, Taiwan, ROC)、染井 一寛(一般財団法人地域地盤環境研究所)


10:00 〜 10:15

[SSS04-05] Characterization of Earthquake Sources in Diverse Tectonic Settings

*Rachel E Abercrombie1 (1.Boston University, Boston, USA)

キーワード:earthquake, stress drop, source complexity

Detailed analysis of well-recorded earthquake sequences, tectonic and induced, has the potential to reveal the relative influence of multiple processes on earthquake nucleation and rupture propagation. High precision relocations enable mapping of seismicity migration rates, indicative of fluid or aseismic forcing. Combined with focal mechanisms, the relocations reveal the active structures and their relative stress states. Source analysis provides information about the finite rupture extents, and rupture directions, which are needed to constrain earthquake interactions and triggering. Earthquake stress drop, rupture propagation direction, and even source complexity may depend on local conditions resolvable by seismicity characteristics. However, all these parameters are hard to resolve unambiguously because of the limited frequency range of most recordings, and the need to remove the effects of attenuation and other path effects. My recent work on tectonic and induced earthquakes in western and central United States and beyond, with many coauthors, has provided insights into resolution and uncertainties. It has also revealed spatial and temporal variations of stress drop in both swarms and repeating earthquake sequences that may help us understand the factors governing earthquake rupture. I will summarize some of these recent results, and discuss their implications.