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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| 格式: | Article |
| 語言: | English |
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2017
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| 在線閱讀: | https://hdl.handle.net/10356/80744 http://hdl.handle.net/10220/42232 |
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