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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

  • Czech description

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

Result continuities

  • Project

  • 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

  • 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