Geoelectrical and geological structure of the crust in Western Slovakia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F14%3A00430185" target="_blank" >RIV/67985530:_____/14:00430185 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1007/s11200-013-0491-9" target="_blank" >http://dx.doi.org/10.1007/s11200-013-0491-9</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s11200-013-0491-9" target="_blank" >10.1007/s11200-013-0491-9</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Geoelectrical and geological structure of the crust in Western Slovakia

Popis výsledku v původním jazyce

Electrical resistivity of the Earth?s crust is sensitive to a wide range of petrological and physical parameters, and it particularly clearly indicates crustal zones that have been tectonically or thermodynamically disturbed. A complex geological structure of the Alpine nappe system, remnants of older Hercynian units and Neogene block tectonics in Western Slovakia has been a target of recent magnetotelluric investigations which made a new and more precise identification of the crustal structural elements of the Western Carpathians possible. A NW-SE magnetotelluric profile, 150 km long, with 30 broad-band and 3 long- period magnetotelluric sites, was deployed, crossing the major regional tectonic elements listed from the north: Brunia (as a part of theEuropean platform), Outer Carpathian Flysch, Klippen Belt, blocks of Penninic or Oravicum crust, Tatricum and Veporicum.

Název v anglickém jazyce

Geoelectrical and geological structure of the crust in Western Slovakia

Popis výsledku anglicky

Electrical resistivity of the Earth?s crust is sensitive to a wide range of petrological and physical parameters, and it particularly clearly indicates crustal zones that have been tectonically or thermodynamically disturbed. A complex geological structure of the Alpine nappe system, remnants of older Hercynian units and Neogene block tectonics in Western Slovakia has been a target of recent magnetotelluric investigations which made a new and more precise identification of the crustal structural elements of the Western Carpathians possible. A NW-SE magnetotelluric profile, 150 km long, with 30 broad-band and 3 long- period magnetotelluric sites, was deployed, crossing the major regional tectonic elements listed from the north: Brunia (as a part of theEuropean platform), Outer Carpathian Flysch, Klippen Belt, blocks of Penninic or Oravicum crust, Tatricum and Veporicum.

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

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Studia geophysica et geodaetica

ISSN

0039-3169

e-ISSN

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Svazek periodika

58

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

16

Strana od-do

473-488

Kód UT WoS článku

000340216900008

EID výsledku v databázi Scopus

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