Abstract
Regions where the continental lithosphere is slowly deforming may be perceived as stable because they are far away from active plate boundaries, but these regions can and do experience large earthquakes. The lithosphere is relatively cool and thick in these areas, so earthquakes can propagate deeper than in more active regions and have large magnitudes. Because these earthquakes are rare, however, surrounding populations may not be well prepared and thus face significant hazard. Therefore, it is important for these slowly deforming regions to be well characterized.
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 callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
