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Towards monitoring the englacial fracture state using virtual-reflector seismology
In seismology, coda wave interferometry (CWI) is an effective tool to monitor time-lapse changes ...
F Lindner, C Weemstra, F Walter, C Hadziioannou | Journal: Geophysical Journal International | Volume: 214 | Year: 2018 | First page: 825 | Last page: 844 | doi: https://doi.org/10.1093/gji/ggy156
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Short- and Long-Term Variations in the Reykjanes Geothermal Reservoir From Seismic Noise Interferometry
The Reykjanes Geothermal System (RGS) is a high-temperature geothermal system located on the Reyk...
Pilar Sánchez-Pastor, Anne Obermann, Martin Schimmel, Cornelis Weemstra, Arie Verdel, Philippe Jousset | Journal: Geophysical Research Letters | Volume: 46 | Year: 2019 | First page: 5788 | Last page: 5798 | doi: https://doi.org/10.1029/2019GL082352
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Decades of subsidence followed by rapid uplift: Insights from microgravity data at Askja Volcano, Iceland
In August 2021, Askja volcano in Iceland returned to the spotlight after a sudden onset of rapid ...
M Koymans, E de Zeeuw-van Dalfsen, J Sepúlveda, L Evers, J Giniaux, R Grapenthin, A Hooper, B Ófeigsson, F Sigmundsson, Y Yang | Journal: Journal of Volcanology and Geothermal Research | Volume: 442 | Year: 2023 | doi: 10.1016/j.jvolgeores.2023.107890
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Microgravity Change During the 2008–2018 Kı̄lauea Summit Eruption: Nearly a Decade of Subsurface Mass Accumulation
Results from nine microgravity campaigns from Kı̄lauea, Hawaiʻi, spanning most of the volcano's 2...
M Koymans, E de Zeeuw‐van Dalfsen, L Evers, M Poland | Journal: Journal of Geophysical Research: Solid Earth | Volume: 127 | Year: 2022 | doi: 10.1029/2022JB024739
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Introduction to the Special Section on Seismoacoustics and Seismoacoustic Data Fusion
A variety of geophysical hazards (e.g., volcanic activity, earthquakes, mass movements, marine st...
FK Dannemann Dugick, JW Bishop, L Martire, AM Iezzi, JD Assink, Q Brissaud, S Arrowsmith | Journal: Bulletin of the Seismological Society of America | Year: 2023 | doi: https://doi.org/10.1785/0120230049
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