Stress-driven fluid flow controls long-term megathrust strength and deep accretionary dynamics
Abstract
The heterogeneity of frictional strength along the megathrust earthquake zone critically controls plate coupling and long-term subduction dynamics. However, the persistence and distribution of high-friction segments through space and time remain poorly constrained. Here, we show that accretion processes, such as tectonic underplating (i.e., basal accretion of material below the fore-arc region), can be used as a proxy to characterize the...
Paper Details
Title
Stress-driven fluid flow controls long-term megathrust strength and deep accretionary dynamics
Published Date
Jul 4, 2019
Journal
Volume
9
Issue
1
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