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Temporal Magnetotellurics Reveals Mechanics of the 2012 Mount Tongariro, NZ, Eruption

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    SYSNO ASEP0525107
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleTemporal Magnetotellurics Reveals Mechanics of the 2012 Mount Tongariro, NZ, Eruption
    Author(s) Hill, Graham J. (GFU-E) ORCID
    Bibby, H. M. (NZ)
    Peacock, J. (US)
    Wallin, E. L. (US)
    Ogawa, Y. (JP)
    Caricchi, L. (CH)
    Keys, H. (NZ)
    Bennie, S. L. (NZ)
    Avram, Y. (CA)
    Article numbere2019GL086429
    Source TitleGeophysical Research Letters. - : Wiley - ISSN 0094-8276
    Roč. 47, č. 8 (2020)
    Number of pages9 s.
    Publication formPrint - P
    Languageeng - English
    CountryUS - United States
    Keywordsmagnetotellurics ; Taupo Volcanic Zone ; eruption dynamics ; Tongariro
    Subject RIVDE - Earth Magnetism, Geodesy, Geography
    OECD categoryGeology
    Method of publishingOpen access
    Institutional supportGFU-E - RVO:67985530
    UT WOS000530332600006
    EID SCOPUS85083989224
    DOI10.1029/2019GL086429
    AnnotationMonitoring dynamics of volcanic eruptions with geophysics is challenging. In August and November 2012, two small eruptions from Mount Tongariro provided a unique opportunity to image subsurface changes caused by the eruptions. A detailed magnetotelluric survey of the Tongariro volcanic complex completed prior to the eruption (2008-2010) provides the preeruption structure of the magmatic system. A subset of the initial measurement locations was reoccupied in June 2013. Significant changes were observed in phase tensor data at sites close to the eruptive center. Although subsurface electrical resistivity changed, the geometry of the preeruptive reservoir did not. These subsurface resistivity variations are interpreted as being predominantly caused by interaction of partial melt and the overlying brine layer causing volume reduction of the brine layer through phreatic eruption. The ability to detect significant changes associated with the magma reservoir suggests that magnetotellurics can be a valuable volcano monitoring tool.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2021
    Electronic addresshttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2019GL086429
Number of the records: 1  

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