Depth‐Dependent Slow Earthquakes Controlled by Temperature Dependence of Brittle‐Ductile Transitional Rheology

Depth‐Dependent Slow Earthquakes Controlled by Temperature Dependence of Brittle‐Ductile Transitional Rheology

Abstract The discovery of slow earthquakes illuminates the existence of a strange depth dependence of seismogenesis, which contradicts the common understanding of smooth brittle/seismic‐ductile/aseismic transition as going deeper into the earth's surface layers. However, within the transitional...

Cur síos iomlán

Sonraí bibleagrafaíochta
Príomhchruthaitheoirí: Ryosuke Ando, Kohtaro Ujiie, Naoki Nishiyama, Yasushi Mori
Formáid: Alt
Teanga:English
Foilsithe / Cruthaithe: Wiley 2023-03-01
Sraith:Geophysical Research Letters
Ábhair:
slow earthquakes
brittle‐ductile transition
mechanical model
simulation
geology
earthquake source physics
Rochtain ar líne:https://doi.org/10.1029/2022GL101388

Ar líne

https://doi.org/10.1029/2022GL101388

Míreanna comhchosúla