A silent slip event on the deeper Cascadia subduction interface.
about
Connecting slow earthquakes to huge earthquakes.Recurrent slow slip event likely hastened by the 2011 Tohoku earthquake.Reflection signature of seismic and aseismic slip on the northern Cascadia subduction interface.Implications for prediction and hazard assessment from the 2004 Parkfield earthquake.Recurring and triggered slow-slip events near the trench at the Nankai Trough subduction megathrust.Earthquake and tsunami forecasts: relation of slow slip events to subsequent earthquake rupture.Modeling fast and slow earthquakes at various scales.Tidal modulation of nonvolcanic tremor.Slow slip near the trench at the Hikurangi subduction zone, New Zealand.Resonant slow fault slip in subduction zones forced by climatic load stress.Geophysics. Migrating tremor off southern Kyushu as evidence for slow slip of a shallow subduction interface.Earthquakes triggered by silent slip events on Kīlauea volcano, Hawaii.Rheological separation of the megathrust seismogenic zone and episodic tremor and slip.A wide depth distribution of seismic tremors along the northern Cascadia margin.Acoustic-Friction Networks and the Evolution of Precursor Rupture Fronts in Laboratory Earthquakes.Shallow very-low-frequency earthquakes accompany slow slip events in the Nankai subduction zone.Revealing the cluster of slow transients behind a large slow slip event.Interseismic coupling and seismic potential along the Central Andes subduction zoneSimulation of slip transients and earthquakes in finite thickness shear zones with a plastic formulationRapid tremor migration and pore-pressure waves in subduction zonesSlow earthquakes, preseismic velocity changes, and the origin of slow frictional stick-slipPropagation of slow slip leading up to the 2011 M(w) 9.0 Tohoku-Oki earthquakeSubducting slab ultra-slow velocity layer coincident with silent earthquakes in southern MexicoEarthquakes: a movement in four parts?Tiny intraplate earthquakes triggered by nearby episodic tremor and slip in CascadiaRole of multiscale heterogeneity in fault slip from quasi-static numerical simulationsBrittle and ductile friction and the physics of tectonic tremorComplex evolution of transient slip derived from precise tremor locations in western Shikoku, JapanCharacterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New ZealandTriggered tremor sweet spots in AlaskaProbing the slip-weakening mechanism of earthquakes with electrical conductivity: Rapid transition from asperity contact to gouge comminutionMantle hydration and Cl-rich fluids in the subduction forearcTidal modulation of continuous nonvolcanic seismic tremor in the Chile triple junction regionRegionalPwave velocity structure of the Northern Cascadia Subduction ZoneSlow slip events and the 2016 Te Araroa M w 7.1 earthquake interaction: Northern Hikurangi subduction, New ZealandMapping subduction interface coupling using magnetotellurics: Hikurangi margin, New ZealandTectonic Stacking of HP/LT Metamorphic Rocks in Accretionary Wedges and the Role of Shallowing Slab-Mantle DecouplingA geodetic matched filter search for slow slip with application to the Mexico subduction zoneAn aseismic slip transient on the North Anatolian FaultThe Boso slow slip events in 2007 and 2011 as a driving process for the accompanying earthquake swarm
P2860
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P2860
A silent slip event on the deeper Cascadia subduction interface.
description
2001 nî lūn-bûn
@nan
2001 թուականի Ապրիլին հրատարակուած գիտական յօդուած
@hyw
2001 թվականի ապրիլին հրատարակված գիտական հոդված
@hy
2001年の論文
@ja
2001年論文
@yue
2001年論文
@zh-hant
2001年論文
@zh-hk
2001年論文
@zh-mo
2001年論文
@zh-tw
2001年论文
@wuu
name
A silent slip event on the deeper Cascadia subduction interface.
@ast
A silent slip event on the deeper Cascadia subduction interface.
@en
type
label
A silent slip event on the deeper Cascadia subduction interface.
@ast
A silent slip event on the deeper Cascadia subduction interface.
@en
prefLabel
A silent slip event on the deeper Cascadia subduction interface.
@ast
A silent slip event on the deeper Cascadia subduction interface.
@en
P2093
P356
P1433
P1476
A silent slip event on the deeper Cascadia subduction interface.
@en
P2093
P304
P356
10.1126/SCIENCE.1060152
P407
P577
2001-04-19T00:00:00Z