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
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DOI - Digital Object Identifier
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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
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Result continuities
Project
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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
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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
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EID of the result in the Scopus database
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