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Shallow slow slip events have been well documented offshore Gisborne at the northern Hikurangi subduction margin, New Zealand, and are associated with tectonic tremor downdip of the slow slip patch and increases in local microseismicity.
Schwartz, S.Y. +23 more
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Single page posterMany subduction zones worldwide are known to host devastating large earthquakes, such as the 2011 M9 Tohoku-Oki earthquake. In addition to fast, seismic slip many subduction zones also host slow, largely aseismic slip.
Baltay, Annemarie, Littel, Geena
core
In the Bungo Channel along the Nankai Trough, southwest Japan, long-term slow slip events (LSSEs) of about $${M}_{\text{w}}$$ M w 6–7 and lasting 6–12 months occur at several-year intervals at the base of the seismogenic zone.
Fuyuki Hirose, Akio Kobayashi
doaj +1 more source
An edited version of this paper was published by AGU. Copyright (2010) American Geophysical Union.Tectonic tremor has been recorded at many subduction zones, including the Nankai, Cascadia, Mexican, and Alaskan subduction zones. This study, the first to
Creager, K. C. +7 more
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International audienceSubduction megathrusts release stress not only seismically through earthquakes, but also through creep and transient slow deformation, called slow slip events (SSEs).
Moreno, Marcos +6 more
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We use a prestack depth migration reflection image and magnetic anomaly data across the northern Hikurangi subduction zone, New Zealand, to constrain plate boundary structure and geometry of a subducting seamount in a region of shallow slow slip and ...
Daniel H. N. Barker +6 more
doaj +1 more source
Brittle and ductile friction and the physics of tectonic tremor [PDF]
Eric G. Daub +3 more
openaire +1 more source
We have constructed an automated routine to identify prominent bursts of tectonic tremor and locate their source region during time periods of raised amplitude in the tremor passband.
Boyarko, D. C. +4 more
core +1 more source
Volcanic tremor at Mt Vesuvius associated with low frequency shear failures
Mt Vesuvius has been dormant since the eruption occurred in 1944, after which the conduit closed and the volcano entered a quiescent state. Only a minor seismic activity, characterized by low magnitude volcano-tectonic (VT) earthquakes, testifies that ...
La Rocca, Mario, Galluzzo, Danilo
core +2 more sources

