Ring Fault Slip Reversal at Bárðarbunga Volcano, Iceland: Seismicity During Caldera Collapse and Re-Inflation 2014–2018

<jats:title>Abstract</jats:title><jats:p>Microearthquakes reveal the kinematics of the Bárðarbunga caldera ring fault; during the 2014–2015 rifting event and gradual caldera collapse, and its subsequent, ongoing re‐inflation. Tightly constrained focal mechanisms during re‐inflation...

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Bibliographic Details
Main Authors: Glastonbury-Southern, E, Winder, T, White, RS, Brandsdóttir, B
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2022
Subjects:
Baroarbunga
Holuhraun
caldera collapse
microearthquakes
earthquake mechanisms
Iceland
Online Access:https://www.repository.cam.ac.uk/handle/1810/342738
https://doi.org/10.17863/CAM.90151
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Summary:<jats:title>Abstract</jats:title><jats:p>Microearthquakes reveal the kinematics of the Bárðarbunga caldera ring fault; during the 2014–2015 rifting event and gradual caldera collapse, and its subsequent, ongoing re‐inflation. Tightly constrained focal mechanisms during re‐inflation have reversed phase arrival polarities from events during the caldera collapse. Thus, the inner side of the steeply dipping northern caldera faults (averaging 81 ± 8°) has been moving upwards during the post‐eruptive period. Both precise relative relocations of the seismicity and fault plane solutions confirm that this is due to slip reversal on the same ring fault structure.</jats:p>

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