Recent geodynamic and geomorphological analyses of the Diendorf?Čebín Tectonic Zone, Czech Republic

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F13%3A00394168" target="_blank" >RIV/68145535:_____/13:00394168 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216305:26110/13:PU107618

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.tecto.2013.04.008" target="_blank" >http://dx.doi.org/10.1016/j.tecto.2013.04.008</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.tecto.2013.04.008" target="_blank" >10.1016/j.tecto.2013.04.008</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Recent geodynamic and geomorphological analyses of the Diendorf?Čebín Tectonic Zone, Czech Republic

Popis výsledku v původním jazyce

The Diendorf?Čebín Tectonic Zone (DCTZ) located within the south-eastern margin of the Bohemian Massif is a complex Paleozoic structure reactivated during several phases of unequal thrusting of the Alpine?Carpathian orogenic blocks over the European Platformin the Neogene and Quaternary periods. Recent movement tendencies in its area have been studied through analyses of and correlations between regional geophysical fields, geomorphological phenomena and geodetic monitoring processed on the current geological background. The gravity and magnetic information complemented by data from deep seismic sections along with current GPS velocities documented a dominant transcurrent character of this zone with well-developed extensive upward branching negative flower-structure. The geomorphological data, including information on topolineament framework, fluvial system, distribution of flat surfaces and topographic depressions, pattern of repeated similar landforms, and other related landscape fea

Název v anglickém jazyce

Recent geodynamic and geomorphological analyses of the Diendorf?Čebín Tectonic Zone, Czech Republic

Popis výsledku anglicky

The Diendorf?Čebín Tectonic Zone (DCTZ) located within the south-eastern margin of the Bohemian Massif is a complex Paleozoic structure reactivated during several phases of unequal thrusting of the Alpine?Carpathian orogenic blocks over the European Platformin the Neogene and Quaternary periods. Recent movement tendencies in its area have been studied through analyses of and correlations between regional geophysical fields, geomorphological phenomena and geodetic monitoring processed on the current geological background. The gravity and magnetic information complemented by data from deep seismic sections along with current GPS velocities documented a dominant transcurrent character of this zone with well-developed extensive upward branching negative flower-structure. The geomorphological data, including information on topolineament framework, fluvial system, distribution of flat surfaces and topographic depressions, pattern of repeated similar landforms, and other related landscape fea

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DE - Zemský magnetismus, geodesie, geografie

OECD FORD obor

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Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2013

Kód důvěrnosti údajů

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

Název periodika

Tectonophysics

ISSN

0040-1951

e-ISSN

—

Svazek periodika

599

Číslo periodika v rámci svazku

25. červen 2013

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

22

Strana od-do

45-66

Kód UT WoS článku

000321231800004

EID výsledku v databázi Scopus

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