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On the interpretation of normal and inverse magnetic fabric in dikes: Examples from the Eger Graben, NW Bohemian Massif

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    SYSNO ASEP0321769
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleOn the interpretation of normal and inverse magnetic fabric in dikes: Examples from the Eger Graben, NW Bohemian Massif
    TitlePříspěvek k interpretaci normální a inverzní magnetické stavby na příkladu oháreckého riftu, sz. Českého masivu
    Author(s) Chadima, Martin (GLU-S) RID, SAI
    Cajz, Vladimír (GLU-S) RID, SAI, ORCID
    Týcová, P. (CZ)
    Source TitleTectonophysics. - : Elsevier - ISSN 0040-1951
    Roč. 466, 1-2 (2009), s. 47-63
    Number of pages17 s.
    Publication formWWW - WWW
    Languageeng - English
    CountryNL - Netherlands
    Keywordsanisotropy of magnetic remanence ; anisotropy of magnetic susceptibility ; EBSD ; Lattice prefered orientation ; multifunkction Kappabridge
    Subject RIVDE - Earth Magnetism, Geodesy, Geography
    R&D ProjectsIAA300130612 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000264470600005
    EID SCOPUS59949087726
    DOI10.1016/j.tecto.2008.09.005
    AnnotationNormal or inverse fabric in dikes may either reflect the presence of multi-domain (MD)/single-domain (SD) grains or it may result from different orientation mechanisms of magnetic minerals in magmas of different viscosities. The ambiguity in physical vs. geological cause of normal/inverse magnetic fabric must be answered before any successful geological interpretation of magnetic fabric can be made. In order to address this problem, we studied magnetic fabric of selected dikes associated with the SW–NE trending Eger Graben (NW Bohemian Massif). The type of magnetic fabric is lithology-dependent: normal magnetic fabric was found in bostonite and trachybasalt dikes, inverse magnetic fabric was found in camptonite dikes. It is suggested to use preferably anisotropy of magnetic remanence as it reflects the ‘true’ rock fabric more accurately than AMS fabric.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2009
Number of the records: 1  

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