Seismic Amplitude Ratio Analysis of the 2014-2015 Bárðarbunga-Holuhraun Dike Propagation and Eruption

Magma is transported in brittle rock through dikes and sills. This movement may be accompanied by the release of seismic energy that can be tracked from the Earth's surface. Locating dikes and deciphering their dynamics is therefore of prime importance in understanding and potentially forecasti...

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Bibliographic Details
Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Caudron, Corentin, White, Robert S., Green, Robert G., Woods, Jennifer, Agustsdottir, Thorbjorg, Donaldson, Clare, Greenfield, Tim, Rivalta, Eleonora, Brandsdóttir, Bryndís
Other Authors: Jarðvísindastofnun (HÍ), Institute of Earth Sciences (UI), Verkfræði- og náttúruvísindasvið (HÍ), School of Engineering and Natural Sciences (UI), Háskóli Íslands, University of Iceland
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2018
Subjects:
Volcanology
Seismology
Magma migration
Dike propagation
Bárðarbunga
Holuhraun
Eldfjallafræði
Jarðskjálftafræði
Eldgos
Hraun
Bergkvika
Berggangar
Bár
Iceland
Online Access:https://hdl.handle.net/20.500.11815/672
https://doi.org/10.1002/2017JB014660
Description
Summary:Magma is transported in brittle rock through dikes and sills. This movement may be accompanied by the release of seismic energy that can be tracked from the Earth's surface. Locating dikes and deciphering their dynamics is therefore of prime importance in understanding and potentially forecasting volcanic eruptions. The Seismic Amplitude Ratio Analysis (SARA) method aims to track melt propagation using the amplitudes recorded across a seismic network without picking the arrival times of individual earthquake phases. This study validates this methodology by comparing SARA locations (filtered between 2 and 16 Hz) with the earthquake locations (same frequency band) recorded during the 2014–2015 Bár urn:x-wiley:jgrb:media:jgrb52508:jgrb52508-math-0003arbunga‐Holuhraun dike intrusion and eruption in Iceland. Integrating both approaches also provides the opportunity to investigate the spatiotemporal characteristics of magma migration during the dike intrusion and ensuing eruption. During the intrusion SARA locations correspond remarkably well to the locations of earthquakes. Several exceptions are, however, observed. (1) A low‐frequency signal was possibly associated with a subglacial eruption on 23 August. (2) A systematic retreat of the seismicity was also observed to the back of each active segment during stalled phases and was associated with a larger spatial extent of the seismic energy source. This behavior may be controlled by the dike's shape and/or by dike inflation. (3) During the eruption SARA locations consistently focused at the eruptive site. (4) Tremor‐rich signal close to ice cauldrons occurred on 3 September. This study demonstrates the power of the SARA methodology, provided robust site amplification; Quality Factors and seismic velocities are available. The authors thank both reviewers, the Associate Editor, and the Editor for their insightful comments and suggestions that greatly improved this study. Seismometers were borrowed from the Natural Environment Research Council (NERC) SEIS-UK facility ...

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