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Search for and investigation of volcanoes with gravity surveys

  1. 1.
    SYSNO ASEP0502952
    Document TypeC - Proceedings Paper (int. conf.)
    R&D Document TypeConference Paper
    TitleSearch for and investigation of volcanoes with gravity surveys
    Author(s) Mrlina, Jan (GFU-E) ORCID, RID
    Source TitleEAGE-HAGI 1st Asia Pacific Meeting on Near Surface Geoscience and Engineering. Proceedings. - Red Hook : Curran, 2018 - ISBN 978-1-5108-6269-2
    Pagess. 324-328
    Number of pages5 s.
    Publication formPrint - P
    ActionEAGE-HAGI Asia Pacific Meeting on Near Surface Geoscience and Engineering /1./
    Event date09.04.2018 - 13.04.2018
    VEvent locationYogyakarta
    CountryID - Indonesia
    Event typeWRD
    Languageeng - English
    CountryUS - United States
    Keywordsgravity survey ; volcano monitoring ; volcanic structure
    Subject RIVDC - Siesmology, Volcanology, Earth Structure
    OECD categoryVolcanology
    R&D ProjectsLM2010008 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    LM2015079 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportGFU-E - RVO:67985530
    AnnotationGeophysical methods, mainly gravimetry and magnetometry, can serve as suitable tools for location of unknown hidden volcanic structures that are not expressed by any typical topographic features. These may be e.g. diatremes and maars with eroded scoria cones or rims of tuff/tephra material, as well as lava flows. Gravity survey may reveal significant negative anomalies due to low density of the filling of volcanic vents, or positive anomalies over the bodies of compact lava accumulation. Magnetometry would rather show positive anomalies related to most of the volcanic structures due to high content of magnetic minerals in the volcanic rocks (except acid trachytes/phonolites/rhyolites). Geophysical surveys should therefore form part of any investigation of volcanic fields where some unknown volcanoes may still be expected. Gravity monitoring can reveal hidden mass and fluids movement in a volcano interior, and can therefore contribute to the hazard control at regions with active volcanoes.
    WorkplaceGeophysical Institute
    ContactHana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
    Year of Publishing2019
Number of the records: 1  

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