Long-lived shallow slow-slip events on the Sunda megathrust

During most of the time between large earthquakes at tectonic plate boundaries, surface displacement time series are generally observed to be linear. This linear trend is interpreted as a result of steady stress accumulation at frictionally locked asperities on the fault interface. However, due to t...

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Bibliographic Details
Main Authors: Mallick, Rishav, Meltzner, Aron J., Tsang, Louisa L. H., Lindsey, Eric Ostrom, Feng, Lujia, Hill, Emma M.
Other Authors: Asian School of the Environment
Format: Article
Language:English
Published: 2021
Subjects:
Online Access:https://hdl.handle.net/10356/152990
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Institution: Nanyang Technological University
Language: English