Seismic activity and deep conductivity structure of the Eastern Carpathians
Autor: | Lesya Nazarevych, Svetlana Kováčiková, Josef Pek, I.M. Logvinov, Victor Tarasov, Pavel Kalenda, A.V. Nazarevych |
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Rok vydání: | 2016 |
Předmět: |
010504 meteorology & atmospheric sciences
Crust Active fault Conductivity Induced seismicity 010502 geochemistry & geophysics 01 natural sciences Geophysics Geochemistry and Petrology Magnetotellurics Vertical direction Structural geology Joint (geology) Geology Seismology 0105 earth and related environmental sciences |
Zdroj: | Studia Geophysica et Geodaetica. 60:280-296 |
ISSN: | 1573-1626 0039-3169 |
DOI: | 10.1007/s11200-014-0942-y |
Popis: | 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 km. 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. |
Databáze: | OpenAIRE |
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