Abstract
Earthquakes can occur at great depths in the Earth, within subducting tectonic plates. Deformation experiments suggest these deep earthquakes can be triggered by localized heating of the slabs under high pressures.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
