DOI: 10.1016/j.epsl.2018.08.046
Scopus记录号: 2-s2.0-85053073522
论文题名: Dynamic triggering of shallow slip on forearc faults constrained by monitoring surface displacement with the IPOC Creepmeter Array
作者: Victor P. ; Oncken O. ; Sobiesiak M. ; Kemter M. ; Gonzalez G. ; Ziegenhagen T.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2018
卷: 502 起始页码: 57
结束页码: 73
语种: 英语
英文关键词: Atacama Fault System
; creepmeter array
; dynamic triggering
; seismic energy density
; shallow fault slip
Scopus关键词: Earthquakes
; Surface measurement
; Surface waves
; Volcanoes
; creepmeter array
; Dynamic triggering
; Fault system
; Seismic energy
; Shallow faults
; Fault slips
; Chile earthquake 2010
; displacement
; earthquake epicenter
; fault slip
; monitoring
; seismic wave
; subduction zone
; Atacama
; Chile
英文摘要: The Mw=8.8 Maule Earthquake of February 27, 2010, remotely triggered minor surface displacement along the Atacama Fault System in Northern Chile located 1500–1800 km from the epicenter. Here we present evidence that surface displacement events recorded by the IPOC (Integrated Plate Boundary Observatory in N-Chile) Creepmeter Array are related to earthquakes on the underlying subduction zone interface or to large earthquakes around the world. Our observations document dynamic triggering of shallow slip on faults in a forearc setting. Continuous monitoring revealed that up to 30 displacement events per year occur on the monitored fault segments, >90% of them triggered by earthquakes in the near or far field synchronous to the passage of the seismic wave. We can clearly attribute far field triggering to the passage of the surface wave and near field triggering to the passage of the body wave. The most distant triggered displacement event monitored occurred after the 2011, Mw=9.0 Tohoku-Oki Earthquake located 16 468 km away following the passage of large amplitude SS waves. Comparing the triggered displacement events with other triggered phenomena like seismicity, volcanic eruptions, hydrological changes as well as with data from the California Creepmeter Array we find that the seismic energy density appropriately describes a magnitude–distance scaling relationship of slip triggering. Finally, the observed surface displacement is found to not occur by continuous creep, but rather through nearly exclusively discrete displacement events. © 2018 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109655
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: Helmholtz-Zentrum Potsdam, Deutsches GeoForschungsZentrum (GFZ) Potsdam, Potsdam, 14473, Germany; Institute of Geophysics, Polish Academy of Sciences, Krakow, 30239, Poland; Departamento de Ciencias Geologicas, Universidad Catolica del Norte, Avenida Angamos 0610, Antofagasta, Chile
Recommended Citation:
Victor P.,Oncken O.,Sobiesiak M.,et al. Dynamic triggering of shallow slip on forearc faults constrained by monitoring surface displacement with the IPOC Creepmeter Array[J]. Earth and Planetary Science Letters,2018-01-01,502