Rapid tremor migration and pore-pressure waves in subduction zones

Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone processes on the plate interface. Recent observations have revealed a large diversity of RTM patterns that are always associated with aseismic, shear strain at the interface. Small unstable asperities embedded...

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Bibliographic Details
Published in:Nature communications 2018-07, Vol.9 (1), p.2900-13, Article 2900
Main Authors: Cruz-Atienza, Víctor M., Villafuerte, Carlos, Bhat, Harsha S.
Format: Article
Language:English
Subjects:
704/2151/508
704/2151/562
Computational fluid dynamics
Earthquakes
Elastic waves
Fluid pressure
Humanities and Social Sciences
Migration
multidisciplinary
Pressure
Science
Science (multidisciplinary)
Seismic activity
Shear strain
Shear zone
Spatial variations
Subduction (geology)
Tremors
Wave propagation
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Summary:Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone processes on the plate interface. Recent observations have revealed a large diversity of RTM patterns that are always associated with aseismic, shear strain at the interface. Small unstable asperities embedded in the stable shear zone are thus believed to originate tremor radiation during migration. Tectonic tremors have been recognized to occur where overpressured fluids exist. Spatial variations of fluid pressure may lead to non-linear diffusion processes with potentially large implications in tremor generation. Here, we show that pore-pressure waves are likely to exist in the plate interface, propagating with speeds and pathways similar to RTMs observed in different subduction zones including Guerrero, Mexico, where we introduce new high-resolution tremor locations and a RTM source physical model. These waves may explain the whole hierarchy of RTM patterns by producing transient reductions of the fault strength and thus secondary slip fronts triggering tremor during slow earthquakes. Rapid tremor migration in subduction zones has been associated with aseismic, shear strain at the plate interface. Here, the authors develop a physical model that shows that pore-pressure waves at the plate interface are likely to generate secondary slip fronts triggering rapid tremor migrations with speeds and pathways similar to those observed in subduction zones.
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-018-05150-3