STUDY OF RISK ZONES AT THE BOHEMIAN MASSIF AND WESTERN CARPATHIANS TERRITORY
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216305%3A26110%2F16%3APU117421" target="_blank" >RIV/00216305:26110/16:PU117421 - isvavai.cz</a>
Výsledek na webu
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DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
STUDY OF RISK ZONES AT THE BOHEMIAN MASSIF AND WESTERN CARPATHIANS TERRITORY
Popis výsledku v původním jazyce
Distinctive structures have been ascertained in region of eastern part of the Bohemian Massif and Western Carpathians on the bases of the Remote Sensing, in the past. Their explanation and verification have been not yet realized, even though all structures have regional character and many morphological signs which unambiguously point out recent activity and deformations, including earthquake foci occurence. Among the mentioned structures belong the interpreted non-linear structures - “gravity nappe” in the western part of the Nízké Tatry Mts. and adjacent area of the Slovenské rudohorie Mts., resemble sliding block in the Malé Karpaty Mts., and Ukraine Flysch Carpathians, linear boundaries interpreted as tectonic systems – e.g. Myjava-SubTatra and Hron tectonic zones or Muráň-Malcov and Transgemeric tectonic zones. Their important role in neotectonic plane of the Western Carpathians was confirmed by newly processed GNSS data from permanent stations and epoch campaigns realized during last decades in mentioned area. On two chosen examples from the area of Slovakian Carpathians there are presented the interpreted results verified on the bases of satellite images, morphological, geophysical and GPS data evaluation.
Název v anglickém jazyce
STUDY OF RISK ZONES AT THE BOHEMIAN MASSIF AND WESTERN CARPATHIANS TERRITORY
Popis výsledku anglicky
Distinctive structures have been ascertained in region of eastern part of the Bohemian Massif and Western Carpathians on the bases of the Remote Sensing, in the past. Their explanation and verification have been not yet realized, even though all structures have regional character and many morphological signs which unambiguously point out recent activity and deformations, including earthquake foci occurence. Among the mentioned structures belong the interpreted non-linear structures - “gravity nappe” in the western part of the Nízké Tatry Mts. and adjacent area of the Slovenské rudohorie Mts., resemble sliding block in the Malé Karpaty Mts., and Ukraine Flysch Carpathians, linear boundaries interpreted as tectonic systems – e.g. Myjava-SubTatra and Hron tectonic zones or Muráň-Malcov and Transgemeric tectonic zones. Their important role in neotectonic plane of the Western Carpathians was confirmed by newly processed GNSS data from permanent stations and epoch campaigns realized during last decades in mentioned area. On two chosen examples from the area of Slovakian Carpathians there are presented the interpreted results verified on the bases of satellite images, morphological, geophysical and GPS data evaluation.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
DE - Zemský magnetismus, geodesie, geografie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2016
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
Družicové metody v geodézii a katastru
ISBN
978-80-86433-59-2
ISSN
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e-ISSN
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Počet stran výsledku
9
Strana od-do
45-53
Název nakladatele
ECON publishing Brno
Místo vydání
Brno
Místo konání akce
Brno
Datum konání akce
5. 2. 2015
Typ akce podle státní příslušnosti
EUR - Evropská akce
Kód UT WoS článku
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