'Non European' paleomagnetic directions from the Carpathian Foredeep at the southern margin of the European plate

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F11%3A00000007" target="_blank" >RIV/00025798:_____/11:00000007 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

'Non European' paleomagnetic directions from the Carpathian Foredeep at the southern margin of the European plate

Popis výsledku v původním jazyce

A paleomagnetic study carried out on 33 geographically distributed localities in the Miocene fill of the nearly 600 km long Moravian and Polish segments of the Carpathian Foredeep revealed an overall, more that 20° CCW rotation of the area. The new paleomagnetic results can be best interpreted in terms of CCW rotation, starting around 17Ma and probably continuing even today. The rotations must have affected not only the sedimentary fill of the Carpathian Foredeep, but also the basement, due to the dextral shift on the NW-SE trending block-bounding faults, observed in the basement as well as in the Miocene sediments. The present evidence for ?non European? paleomagnetic directions north of the Alpine-Carpathian mountain chain together with the previously published indications seriously question the rigidity of the European plate during the last 20Ma, at least near the thrust front of the Alps and Carpathians.

Název v anglickém jazyce

'Non European' paleomagnetic directions from the Carpathian Foredeep at the southern margin of the European plate

Popis výsledku anglicky

A paleomagnetic study carried out on 33 geographically distributed localities in the Miocene fill of the nearly 600 km long Moravian and Polish segments of the Carpathian Foredeep revealed an overall, more that 20° CCW rotation of the area. The new paleomagnetic results can be best interpreted in terms of CCW rotation, starting around 17Ma and probably continuing even today. The rotations must have affected not only the sedimentary fill of the Carpathian Foredeep, but also the basement, due to the dextral shift on the NW-SE trending block-bounding faults, observed in the basement as well as in the Miocene sediments. The present evidence for ?non European? paleomagnetic directions north of the Alpine-Carpathian mountain chain together with the previously published indications seriously question the rigidity of the European plate during the last 20Ma, at least near the thrust front of the Alps and Carpathians.

Druh

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

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/GETOP%2F08%2FE014" target="_blank" >GETOP/08/E014: Kvantifikace výzdvihu a eroze v Západních Karpatech a přilehlém Českém masívu ve vztahu k transportu sedimentů do aktivních sedimentárních pánví</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Terra Nova

ISSN

0954-4879

e-ISSN

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Svazek periodika

23

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

15

Strana od-do

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Kód UT WoS článku

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EID výsledku v databázi Scopus

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