Slowly migrating tectonic microearthquake swarms in the Icelandic Rift Zone: driven by pore-pressure or aseismic slip transients? (2021)
Attributed to:
Monitoring Magmatism and Intrusion from the Bardabunga Volcano, Iceland
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/egusphere-egu21-15544
Publication URI: http://dx.doi.org/10.5194/egusphere-egu21-15544
Type: Other