Inferring fault rheology from low-frequency earthquakes on the San Andreas
about
Rheological separation of the megathrust seismogenic zone and episodic tremor and slip.The Parkfield tremors reveal slow and fast ruptures on the same asperity.A 15 year catalog of more than 1 million low-frequency earthquakes: Tracking tremor and slip along the deep San Andreas FaultConstraints on the source parameters of low-frequency earthquakes on the San Andreas FaultComplexity of the deep San Andreas Fault zone defined by cascading tremor
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Inferring fault rheology from low-frequency earthquakes on the San Andreas
description
wetenschappelijk artikel
@nl
наукова стаття, опублікована в листопаді 2013
@uk
name
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@en
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@nl
type
label
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@en
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@nl
prefLabel
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@en
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@nl
P2860
P50
P356
P1476
Inferring fault rheology from low-frequency earthquakes on the San Andreas
@en
P2093
Amanda Thomas
P2860
P304
P356
10.1002/2013JB010118
P577
2013-11-01T00:00:00Z