Omori‐like decay of postseismic velocities following continental earthquakes

Abstract Various mechanisms have been proposed to explain the transient, enhanced surface deformation rates following earthquakes. Unfortunately, these different mechanisms can produce very similar surface deformation patterns leading to difficulty in distinguishing between them. Here we return to t...

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Bibliographic Details
Main Authors: T. Ingleby, T. J. Wright
Format: Article
Language:English
Published: Wiley 2017-04-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2017GL072865
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