Evidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake Source

Evidence of Localized Failure Along Altered Basaltic Blocks in Tectonic Mélange at the Updip Limit of the Seismogenic Zone: Implications for the Shallow Slow Earthquake Source

Abstract Field studies have led to several interpretations on the mechanics behind slow earthquake phenomena downdip of the seismogenic zone. To date, field studies have not examined the shallow subduction interface which may also host slow earthquake phenomena. We examine a subduction mélange exhum...

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Bibliographic Details
Main Authors: Noah John Phillips, Ginta Motohashi, Kohtaro Ujiie, Christie D. Rowe
Format: Article
Language:English
Published: Wiley 2020-07-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
subduction
mélange
slow earthquakes
low‐frequency earthquakes
lithologic heterogeneity
altered basalt
Online Access:https://doi.org/10.1029/2019GC008839

Internet

https://doi.org/10.1029/2019GC008839

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