Shear wave crustal velocity model of the Western Bohemian Massif from Love wave phase velocity dispersion

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F11%3A00357045" target="_blank" >RIV/67985891:_____/11:00357045 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11320/11:10098789
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Shear wave crustal velocity model of the Western Bohemian Massif from Love wave phase velocity dispersion
Original language description
We propose a new quantitative determination of shear wave velocities for distinct geological units in the Bohemian Massif. We have developed a modified version of the classical multiple filtering technique for the frequency-time analysis and we apply itto two-station phase velocity estimation. Two of the profiles crossing the older Moldanubian and Tepla-Barrandian units are characterized by higher velocities of 3.8 km/s in the upper crust while for the Saxothuringian unit we find the velocity slightlylower, around 3.6 km/s at the same depths. We obtain an indication of a shear wave low velocity zone above Moho in the Moldanubian and Tepla-Barrandian units. The area of the Eger Rift (Tepla-Barrandian-Saxothuringian unit contact) is significantly different from all other three units.
Czech name
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Czech description
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Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year
2011
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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