Risk faults in stable crust of the eastern Bohemian Massif identified by integrating GNSS, levelling, geological, geomorphological and geophysical data
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F20%3A10245014" target="_blank" >RIV/61989100:27350/20:10245014 - isvavai.cz</a>
Alternative codes found
RIV/68145535:_____/20:00534723 RIV/00216305:26110/20:PU138070
Result on the web
<a href="https://www.x-mol.com/paper/1249790248625266688?recommendPaper=1234994112922218496" target="_blank" >https://www.x-mol.com/paper/1249790248625266688?recommendPaper=1234994112922218496</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.tecto.2020.228427" target="_blank" >10.1016/j.tecto.2020.228427</a>
Alternative languages
Result language
angličtina
Original language name
Risk faults in stable crust of the eastern Bohemian Massif identified by integrating GNSS, levelling, geological, geomorphological and geophysical data
Original language description
It is difficult to identify and assess the recently active faults, representing a risk factor for key human activities, in the areas of stable crust with slow tectonic deformation and reduced seismicity. We face the problem in the eastern Bohemian Massif (Central European Variscides) at a contact with the Eastern Alpine - Western Carpathian orogenic belt through building its integrated geodynamic model based on the long-term GNSS data cross-checked with the results from existing levelling, geological surveys, geophysical surveys, and a new geomorphological analysis. The model shows differently moving crustal blocks, determining the intervening boundary zones as the main risk regions, where weak earthquakes are also usually concentrated (primarily Diendorf-Čebín Tectonic Zone, Nectava-Konice Fault, Haná Faults, Bělá Fault and Bulhary Fault Shear Zone). The maximum horizontal GNSS differential velocities in the exposed Bohemian Massif reach up to 1.5-2.0 mm.yrMINUS SIGN 1. The up-thrusted segments of the Western Carpathians move individually ~2 mm.yrMINUS SIGN 1. The integration of a number of full-area datasets, corresponding to various dimensions and depth levels of crustal processes, allowed us to highlight the important fault zones as driving elements of regional geodynamics. (C) 2020 Elsevier B.V.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10500 - Earth and related environmental sciences
Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2020
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
785
Issue of the periodical within the volume
20. 6. 2020
Country of publishing house
US - UNITED STATES
Number of pages
24
Pages from-to
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UT code for WoS article
000536204800003
EID of the result in the Scopus database
2-s2.0-85084547466