Decay of aftershock density with distance indicates triggering by dynamic stress.
about
Stress imparted by the great 2004 Sumatra earthquake shut down transforms and activated rifts up to 400 km away in the Andaman Sea.Triggered dynamics in a model of different fault creep regimesAnthropogenic triggering of large earthquakes.Mechanical origin of aftershocks.SEDA: A software package for the Statistical Earthquake Data Analysis.Spatial organization of foreshocks as a tool to forecast large earthquakes.Scaling behavior of the earthquake intertime distribution: influence of large shocks and time scales in the Omori law.Networks of recurrent events, a theory of records, and an application to finding causal signatures in seismicity.Local near instantaneously dynamically triggered aftershocks of large earthquakes.Phase response curves for models of earthquake fault dynamics.Dynamic Weakening by Acoustic Fluidization during Stick-Slip Motion.No evidence of magnitude clustering in an aftershock sequence of nano- and picoseismicity.Clustering analysis of seismicity and aftershock identification.Three-dimensional discrete element modeling of triggered slip in sheared granular media.Acceleration and localization of subcritical crack growth in a natural composite material.Reviewing and visualizing the interactions of natural hazardsStrain waves, earthquakes, slow earthquakes, and afterslip in the framework of the Frenkel-Kontorova modelNetwork of recurrent events for the Olami-Feder-Christensen modelUniversal earthquake-occurrence jumps, correlations with time, and anomalous diffusionEarthquakes: a hand on the aftershock triggerThe January 2010 Efpalion earthquakes (Gulf of Corinth, Central Greece): earthquake interactions and blind normal faultingFitting and goodness-of-fit test of non-truncated and truncated power-law distributionsStructure of earthquake occurrence in space, time and magnitudeAftershocks driven by afterslip and fluid pressure sweeping through a fault-fracture meshTremor reveals stress shadowing, deep postseismic creep, and depth-dependent slip recurrence on the lower-crustal San Andreas fault near ParkfieldTriggered creep as a possible mechanism for delayed dynamic triggering of tremor and earthquakesSystematic assessment of the static stress triggering hypothesis using interearthquake time statisticsThe stress shadow problem in physics-based aftershock forecasting: Does incorporation of secondary stress changes help?Pulverization provides a mechanism for the nucleation of earthquakes at low stress on strong faultsMagnification of mantle resonance as a cause of tectonicsLimitations of rupture forecasting exposed by instantaneously triggered earthquake doubletChange in seismicity along the Japan trench, 1990-2011, and its relationship with seismic couplingChanges in permeability caused by transient stresses: Field observations, experiments, and mechanisms
P2860
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P2860
Decay of aftershock density with distance indicates triggering by dynamic stress.
description
2006 nî lūn-bûn
@nan
2006年の論文
@ja
2006年学术文章
@wuu
2006年学术文章
@zh
2006年学术文章
@zh-cn
2006年学术文章
@zh-hans
2006年学术文章
@zh-my
2006年学术文章
@zh-sg
2006年學術文章
@yue
2006年學術文章
@zh-hant
name
Decay of aftershock density with distance indicates triggering by dynamic stress.
@en
Decay of aftershock density with distance indicates triggering by dynamic stress.
@nl
type
label
Decay of aftershock density with distance indicates triggering by dynamic stress.
@en
Decay of aftershock density with distance indicates triggering by dynamic stress.
@nl
prefLabel
Decay of aftershock density with distance indicates triggering by dynamic stress.
@en
Decay of aftershock density with distance indicates triggering by dynamic stress.
@nl
P2860
P356
P1433
P1476
Decay of aftershock density with distance indicates triggering by dynamic stress
@en
P2093
P2860
P2888
P304
P356
10.1038/NATURE04799
P407
P577
2006-06-01T00:00:00Z
P5875
P6179
1040813306