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

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

Titill: Seismic Amplitude Ratio Analysis of the 2014-2015 Bárðarbunga-Holuhraun Dike Propagation and Eruption
Höfundur: Caudron, Corentin
White, Robert S.
Green, Robert G.
Woods, Jennifer
Agustsdottir, Thorbjorg   orcid.org/0000-0001-5406-0971
Donaldson, Clare
Greenfield, Tim
Rivalta, Eleonora
Brandsdóttir, Bryndís   orcid.org/0000-0002-4018-0697
Útgáfa: 2018-01
Tungumál: Enska
Umfang: 264-276
Háskóli/Stofnun: Háskóli Íslands
University of Iceland
Svið: Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Deild: Jarðvísindastofnun (HÍ)
Institute of Earth Sciences (UI)
Birtist í: Journal of Geophysical Research: Solid Earth;123(1)
ISSN: 2169-9313
DOI: 10.1002/2017JB014660
Efnisorð: Volcanology; Seismology; Magma migration; Dike propagation; Bárðarbunga; Holuhraun; Eldfjallafræði; Jarðskjálftafræði; Eldgos; Hraun; Bergkvika; Berggangar
URI: https://hdl.handle.net/20.500.11815/672

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Caudron, C., White, R. S., Green, R. G., Woods, J., Ágústsdóttir, T., Donaldson, C., . . . Brandsdóttir, B. (2018). Seismic Amplitude Ratio Analysis of the 2014–2015 Bárðarbunga‐Holuhraun Dike Propagation and Eruption. Journal of Geophysical Research: Solid Earth, 123(1), 264-276. doi:doi:10.1002/2017JB014660


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.


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