Seismic Amplitude Ratio Analysis of the 2014–2015 Bárarbunga‐Holuhraun Dike Propagation and Eruption

  • Corentin Caudron
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Robert S. White
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Robert G. Green
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Jennifer Woods
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Thorbjörg Ágústsdóttir
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Clare Donaldson
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Tim Greenfield
    Department of Earth Sciences, Bullard Laboratories University of Cambridge Cambridge UK
  • Eleonora Rivalta
    Helmholtz‐Centre Potsdam ‐ GFZ German Research Centre for Geosciences Potsdam Germany
  • Bryndís Brandsdóttir
    Institute of Earth Sciences University of Iceland Reykjavík Iceland

書誌事項

公開日
2018-01
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1002/2017jb014660
公開者
American Geophysical Union (AGU)

この論文をさがす

説明

<jats:title>Abstract</jats:title><jats:p>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 <jats:inline-graphic xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="graphic/jgrb52508-math-0003.png" xlink:title="urn:x-wiley:jgrb:media:jgrb52508:jgrb52508-math-0003"/>arbunga‐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.</jats:p>

収録刊行物

被引用文献 (3)*注記

もっと見る

問題の指摘

ページトップへ