Contribution of viscoelastic flow in earthquake cycles within the lithosphere-asthenosphere system

Faults slip relaxes lithospheric stress imposed by mantle flow and in turn transfers stress to the ductile regions. The interplay of these systems governs the style of deformation at plate boundaries including the recurrence of seismic events. However, such deep processes remain challenging to incor...

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Bibliographic Details
Main Authors: Lambert, Valère, Barbot, Sylvain
Other Authors: Earth Observatory of Singapore
Format: Journal Article
Language:English
Published: 2017
Subjects:
Online Access:https://hdl.handle.net/10356/80744
http://hdl.handle.net/10220/42232