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Comment to a paper "The origin of high magnetic remanence in the fault pseudotachylites: Theoretical considerations and implication for coseismic electrical currents"

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F06%3A00051128" target="_blank" >RIV/67985831:_____/06:00051128 - isvavai.cz</a>

  • Result on the web

  • DOI - Digital Object Identifier

Alternative languages

  • Result language

    angličtina

  • Original language name

    Comment to a paper "The origin of high magnetic remanence in the fault pseudotachylites: Theoretical considerations and implication for coseismic electrical currents"

  • Original language description

    Authors of the commented paper prescribed natural remanent magnetization (NRM) of pseudotachylites to co-seismic electrical currents. They rule out the Earth magnetic field as being too weak to magnetize pseudotachylites to the sufficient observed NRM intensity. However, the authors show on page 132 that the saturation remanence of pseudotachylites is 11,000 A/m. Listed maximum NRM intensity in their paper is 132 A/m (see page 132). The ration between the NRM intensity and saturation remanence is therefore 0.012. Based on the papers discussing remanence acquired by electric currents (Wasilewski and Kletetschka, 1999) and consideration of geo-magnetically acquired remanent magnetism in rocks and meteorites (Kletetschka et al., 2003, 2004) this ratio falls in the range of (0.01?0.02) that is consistent with remanent magnetization acquired within the geomagnetic field (50,000 nT). Therefore any magnetization by co-seismic currents is not required and appears to be only speculation.

  • Czech name

    Komentář ke článku "Původ vysoké remanence u zlomových pseudotachylitů: teoretické zvážení a implikace coseismickych elektrických proudů"

  • Czech description

    Komentář ke článku "Původ vysoké remanence u zlomových pseudotachylitů: teoretické zvážení a implikace koseismickych elektrických proudů".

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    BM - Solid-state physics and magnetism

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    Z - Vyzkumny zamer (s odkazem do CEZ)

Others

  • Publication year

    2006

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Tectonophysics

  • ISSN

    0040-1951

  • e-ISSN

  • Volume of the periodical

    419

  • Issue of the periodical within the volume

    1-4

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    1

  • Pages from-to

    99-99

  • UT code for WoS article

  • EID of the result in the Scopus database