STUDY OF RISK ZONES AT THE BOHEMIAN MASSIF AND WESTERN CARPATHIANS TERRITORY

Kód výsledku v IS VaVaI

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Výsledek na webu

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DOI - Digital Object Identifier

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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.

Druh

D - Stať ve sborníku

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

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Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2016

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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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