Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge
Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge"
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ABSTRACT 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 km2 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. Access through your institution Buy or subscribe This is a preview of subscription content, access via your institution
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FAQs * Contact customer support SIMILAR CONTENT BEING VIEWED BY OTHERS LONG-LIVED SHALLOW SLOW-SLIP EVENTS ON THE SUNDA MEGATHRUST Article 03 May 2021 GEOLOGICAL CONSTRAINTS ON THE
MECHANISMS OF SLOW EARTHQUAKES Article 23 March 2021 EFFECTS OF EPISODIC SLOW SLIP ON SEISMICITY AND STRESS NEAR A SUBDUCTION-ZONE MEGATHRUST Article Open access 21 December 2021 REFERENCES
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providing the cGPS and seismological data, and AllTerra NZ for additional GPS data. We acknowledge funding support for this work from GNS Science, the Marsden Fund of the Royal Society of
New Zealand, and the NZ Ministry for Business, Innovation, and Employment (MBIE). L.M.W. and N.B. acknowledge support from NSF grants OCE-1551876 and OCE-1551929. We wish to acknowledge the
contribution of the NeSI high-performance computing facilities to the results of this research. New Zealand’s national facilities are provided by the NZ eScience Infrastructure and funded
jointly by NeSI’s collaborator institutions and through MBIE’s Research Infrastructure programme. AUTHOR INFORMATION AUTHORS AND AFFILIATIONS * GNS Science, Lower Hutt, 5011, New Zealand
Laura M. Wallace, Yoshihiro Kaneko, Sigrún Hreinsdóttir, Ian Hamling, Elisabetta D’Anastasio & Bill Fry * University of Texas Institute for Geophysics, Austin, Texas, 78758, USA Laura M.
Wallace * School of Earth and Atmospheric Science, Georgia Tech, Atlanta, Georgia, 30332, USA Zhigang Peng * Department of Geological Sciences, University of Missouri, Columbia, Missouri,
65211, USA Noel Bartlow Authors * Laura M. Wallace View author publications You can also search for this author inPubMed Google Scholar * Yoshihiro Kaneko View author publications You can
also search for this author inPubMed Google Scholar * Sigrún Hreinsdóttir View author publications You can also search for this author inPubMed Google Scholar * Ian Hamling View author
publications You can also search for this author inPubMed Google Scholar * Zhigang Peng View author publications You can also search for this author inPubMed Google Scholar * Noel Bartlow
View author publications You can also search for this author inPubMed Google Scholar * Elisabetta D’Anastasio View author publications You can also search for this author inPubMed Google
Scholar * Bill Fry View author publications You can also search for this author inPubMed Google Scholar CONTRIBUTIONS L.M.W. conceived the study, undertook the TDEFNODE inversions, and led
the writing of the paper. Y.K. undertook the dynamic-stress-change modelling, and contributed to the interpretations and writing of the paper. N.B. was responsible for the Network Inversion
Filter inversions. I.H. undertook the Coulomb stress change modelling. S.H. and E.D’A. undertook processing of the cGPS data. Z.P. and B.F. contributed locations of repeaters during the SSE
and provided seismological expertise and insights into remote triggering of SSEs. CORRESPONDING AUTHOR Correspondence to Laura M. Wallace. ETHICS DECLARATIONS COMPETING INTERESTS The authors
declare no competing financial interests. SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION Supplementary Information (PDF 2736 kb) SUPPLEMENTARY INFORMATION Supplementary Information
(MP4 5283 kb) SUPPLEMENTARY INFORMATION Supplementary Information (MP4 6879 kb) RIGHTS AND PERMISSIONS Reprints and permissions ABOUT THIS ARTICLE CITE THIS ARTICLE Wallace, L., Kaneko, Y.,
Hreinsdóttir, S. _et al._ Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedge. _Nature Geosci_ 10, 765–770 (2017). https://doi.org/10.1038/ngeo3021
Download citation * Received: 10 March 2017 * Accepted: 04 August 2017 * Published: 11 September 2017 * Issue Date: 01 October 2017 * DOI: https://doi.org/10.1038/ngeo3021 SHARE THIS ARTICLE
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Large-scale dynamic triggering of shallow slow slip enhanced by overlying sedimentary wedgeABSTRACT Slow slip events have become recognized in the last decade as an important mode of fault slip, and are most wid...
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