DOI: 10.1038/ngeo3021c
论文题名: Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge
作者: Wallace L.M. ; Kaneko Y. ; Hreinsdóttir S. ; Hamling I. ; Peng Z. ; Bartlow N. ; D'Anastasio E. ; Fry B.
刊名: Nature Geoscience
ISSN: 17520894
出版年: 2017
卷: 10, 期: 10 起始页码: 765
结束页码: 770
语种: 英语
Scopus关键词: earthquake magnitude
; earthquake trigger
; fault slip
; geodetic datum
; microtremor
; seismic wave
; seismicity
; slip
; stress
; subduction zone
; tectonic wedge
; Hikurangi
; New Zealand
; North Island
; Northland
英文摘要: Slow slip events have become recognized in the last decade as an important mode of fault slip, and are most widely observed at subduction zones. Many episodes of tectonic tremor (related to slow slip) have been triggered by distant earthquakes due to dynamic-stress changes from passing seismic waves. However, there are few clear examples of large, geodetically detected slow slip events triggered by distant earthquakes. Here we use analyses of seismic and geodetic data to show that the magnitude 7.8 Kaikōura earthquake in New Zealand in 2016 triggered a large slow slip event between 250 and 600 km away. The slow slip was shallow, at less than 15 km deep, and spanned more than 15,000 km^2 of the central and northern Hikurangi subduction margin. The slow slip initiated immediately after the earthquake, lasted one to two weeks and was accompanied by a swarm of seismicity. We show that changes in dynamic stress in the slow slip source area ranged from 100 to 600 kPa - approximately 1,000 times greater than the static-stress changes of 0.2 to 0.7 kPa. We therefore propose that the slow slip event was triggered by dynamic-stress changes caused by passing seismic waves. Furthermore, the dynamic-stress changes were greatest on the shallow subduction interface, at less than 10 km depth, in a region overlain by a sedimentary wedge that acts as a waveguide, trapping seismic energy and probably promoting triggering of slip. This suggests that shallow slow slip events are more easily triggered by dynamic-stress changes compared with deep events. © 2017 Macmillan Publishers Limited, part of Springer Nature. All rights reserved. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/105693
Appears in Collections: 气候减缓与适应 科学计划与规划
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作者单位: GNS Science, Lower Hutt, New Zealand; University of Texas Institute for Geophysics, Austin, TX, United States; School of Earth and Atmospheric Science, Georgia Tech, Atlanta, United States; Department of Geological Sciences, University of Missouri, Columbia, MO, United States
Recommended Citation:
Wallace L.M.,Kaneko Y.,Hreinsdóttir S.,et al. Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge[J]. Nature Geoscience,2017-01-01,10(10)