Implications of Surface Heat Flux for Shear Stress and Temperature on the Plate Interface Beneath Northern Honshu

Implications of Surface Heat Flux for Shear Stress and Temperature on the Plate Interface Beneath Northern Honshu

Abstract Measurements of surface heat flux from boreholes of the NIED Hi‐net network of seismometers are used to determine temperature and shear stress on the plate interface beneath northern Honshu. At the maximum depth of thrust‐faulting earthquakes, about 60 km, the temperature is 660 ± 240°C and...

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Bibliographic Details
Main Authors: Philip England, Takumi Matsumoto, Simon Wallis
Format: Article
Language:English
Published: Wiley 2024-02-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
plate boundary
shear stress
temperature
earthquake
metamorphism
Online Access:https://doi.org/10.1029/2023GC011285

Internet

https://doi.org/10.1029/2023GC011285

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