Do faults preserve a record of seismic slip: A second opinion
Exhumed fault zones offer insights into deformation processes associated with earthquakes
in unparalleled spatial resolution; however it can be difficult to differentiate seismic slip from …
in unparalleled spatial resolution; however it can be difficult to differentiate seismic slip from …
Inferring earthquake physics and chemistry using an integrated field and laboratory approach
Earthquakes are the result of a combination of (1) physico-chemical processes operating in
fault zones, which allow ruptures to nucleate and rock friction to decrease with increasing …
fault zones, which allow ruptures to nucleate and rock friction to decrease with increasing …
Stable cree** fault segments can become destructive as a result of dynamic weakening
Faults in Earth's crust accommodate slow relative motion between tectonic plates through
either similarly slow slip or fast, seismic-wave-producing rupture events perceived as …
either similarly slow slip or fast, seismic-wave-producing rupture events perceived as …
Coseismic fault rupture at the trench axis during the 2011 Tohoku-oki earthquake
Fault rupture during the 2011 Tohoku-oki earthquake, which generated a huge tsunami, is
thought to have propagated to a shallow part of the subduction zone,,. This observation calls …
thought to have propagated to a shallow part of the subduction zone,,. This observation calls …
Hydrothermal friction experiments on simulated basaltic fault gouge and implications for megathrust earthquakes
Nucleation of earthquake slip at the plate boundary fault (décollement) in subduction zones
has been widely linked to the frictional properties of subducting sedimentary facies …
has been widely linked to the frictional properties of subducting sedimentary facies …
Tsunamigenic potential of the shallow subduction plate boundary inferred from slow seismic slip
H Sugioka, T Okamoto, T Nakamura, Y Ishihara… - Nature …, 2012 - nature.com
At subduction zones, convergence between the two plates at shallow levels was thought to
occur aseismically, accommodated by asiesmic slip along either the megathrust plate …
occur aseismically, accommodated by asiesmic slip along either the megathrust plate …
[HTML][HTML] Pore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone
We use the pore pressure distribution predicted from a waveform tomography (WT) velocity
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …
Tectonic mélange as fault rock of subduction plate boundary
An assemblage of quantitative data sets is examined to evaluate tectonic mélange as a plate
boundary fault rocks in subduction zone. The research object is the latest Cretaceous Mugi …
boundary fault rocks in subduction zone. The research object is the latest Cretaceous Mugi …
Spatiotemporal evolution of slow slip events at the offshore Hikurangi Subduction Zone in 2019 using GNSS, InSAR, and seafloor geodetic data
Detecting crustal deformation during transient deformation events at offshore subduction
zones remains challenging. The spatiotemporal evolution of slow slip events (SSEs) on the …
zones remains challenging. The spatiotemporal evolution of slow slip events (SSEs) on the …
[HTML][HTML] Mixed deformation styles observed on a shallow subduction thrust, Hikurangi margin, New Zealand
Geophysical observations show spatial and temporal variations in fault slip style on shallow
subduction thrust faults, but geological signatures and underlying deformation processes …
subduction thrust faults, but geological signatures and underlying deformation processes …