Results 21 to 30 of about 3,999 (200)
Unraveling Megathrust Seismicity [PDF]
The majority of global seismicity originates at subduction zones, either within the converging plates or along the plate interface. In particular, events with Mw ≥ 8.0 usually occur at the subduction megathrust, which is the frictional interface between subducting and overriding plates.
FUNICIELLO, FRANCESCA +3 more
openaire +3 more sources
Megathrust locking encoded in subduction landscapes. [PDF]
Locked areas of subduction megathrusts are increasingly found to coincide with landscape features sculpted over hundreds of thousand years, yet the mechanisms that underlie such correlations remain elusive. We show that interseismic locking gradients induce increments of irreversible strain across the overriding plate manifested predominantly as ...
Oryan B +5 more
europepmc +6 more sources
Modelling the seismic potential of the Indo-Burman megathrust [PDF]
AbstractThe Indo-Burman arc is the boundary between the India and Burma plates, north of the Sumatra–Andaman subduction zone. The existence of active subduction in the Indo-Burman arc is a debatable issue because the Indian plate converges very obliquely beneath the Burma plate.
Inessa Vorobieva +2 more
openaire +3 more sources
Mega-earthquakes rupture flat megathrusts [PDF]
Mega-earthquakes go the flat way Megathrust faults in subduction zones cause large and damaging earthquakes. Bletery et al. argue that certain geometric features of the subduction zones relate to earthquake size. The key parameter is the curvature of the megathrust.
Bletery, Q. +5 more
openaire +3 more sources
Earthquake Fingerprint of an Incipient Subduction of a Bathymetric High
The resistance of bathymetric highs to subduction results in large‐scale morphological distortions of the outer‐rise, trench, and fore‐arc regions. Once subducted, bathymetric highs induce frictional segmentation along the plate interface that may result
Luigi Passarelli +3 more
doaj +1 more source
The causes for forearc basin and megathrust rupture zone segmentation are controversial. The Nankai forearc, Japan, is separated into five domains based on topography: Enshu, Kumano, Muroto, Tosa, and Hyuga.
G. Kimura +7 more
doaj +1 more source
The roles of quartz and water in controlling unstable slip in phyllosilicate-rich megathrust fault gouges [PDF]
A recent microphysical model for the steady-state frictional behaviour of wet illite/quartz gouges in subduction megathrust settings predicts that velocity-weakening in the seismogenic zone results from a competition between shear-induced dilatation and ...
Christopher J Spiers +8 more
core +2 more sources
Coulomb stress change on inland faults during megathrust earthquake cycle in southwest Japan
In the subduction zone, megathrust earthquakes may modulate the shallow crustal seismicity in the overriding plate. Historical documents indicate the frequent occurrence of large shallow crustal earthquakes in the overriding continental plate 50 years ...
Tsukasa Mitogawa, Takuya Nishimura
doaj +1 more source
Determination of tsunami run-up and golden time in the megathrust subduction zone of the sunda strait segment [PDF]
The Indonesian Disaster Data and Information Management Database state that the tsunami in the Megathrust Subduction Zone of the Sunda Strait Segment is a disaster threat with high impact and loss of life every time it occurs.
Sarikanti Ponangsera Iko +3 more
doaj +1 more source
Feedback between megathrust earthquake cycle and plate convergence. [PDF]
: Over million years, convergence between the Nazca and South America tectonic plates results in Andean orogeny. Over decades/centuries, it fuels the earthquake cycle of the Andean megathrust.
Martin de Blas J +3 more
europepmc +2 more sources

