Seismic activity and deep conductivity structurenof the Eastern Carpathians
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F16%3A00459518" target="_blank" >RIV/67985891:_____/16:00459518 - isvavai.cz</a>
Alternative codes found
RIV/67985530:_____/16:00459518
Result on the web
<a href="http://dx.doi.org/10.1007/s11200-014-0942-y" target="_blank" >http://dx.doi.org/10.1007/s11200-014-0942-y</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s11200-014-0942-y" target="_blank" >10.1007/s11200-014-0942-y</a>
Alternative languages
Result language
angličtina
Original language name
Seismic activity and deep conductivity structurenof the Eastern Carpathians
Original language description
We present results of a study of the seismicity and the geoelectric structure of the Eastern Carpathians. After the evaluation of the seismicity, new methods of processing and analyzing seismic data are developed, which allow constructing an averaged horizontal-layered velocity model of the crust in the Carpathian region of Ukraine, tracing the seismic active faults and localizing the seismic events both in horizontal and in vertical direction with a better precision. For the study of the conductivity structure beneath the Eastern Carpathians, the collected magnetovariation and magnetotelluric data are used. The depth of electrical conductivity anomalies are estimated and the resulting quasi-3D model of the conductivity structure beneath the Carpathians is compared with the seismicity in the depth range of 10 +/- 2.5 mn. The comparison suggests possible geological mechanisms: the seismic events occur mainly in resistive solid rock domains which surround aseismic high-conductivity zones, consisting of at least partially melted material. Aqueous fluids, or a joint effect of several mechanisms, may also play an active role in this distribution.
Czech name
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Czech description
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Classification
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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Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2016
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Studia geophysica et geodaetica
ISSN
0039-3169
e-ISSN
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Volume of the periodical
60
Issue of the periodical within the volume
2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
17
Pages from-to
280-296
UT code for WoS article
000375971300007
EID of the result in the Scopus database
2-s2.0-84960346023