Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F11%3A00368273" target="_blank" >RIV/67985831:_____/11:00368273 - isvavai.cz</a>

Výsledek na webu

<a href="http://gq.pgi.gov.pl/gq/article/view/7602/pdf_23" target="_blank" >http://gq.pgi.gov.pl/gq/article/view/7602/pdf_23</a>

DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland)

Popis výsledku v původním jazyce

In Devonian carbonates of the Holy Cross Mountains (HCM) are documented the record of three individual episodes of remagnetisation. The fold test performed within map-scale folds from central part of the HCM documented early synfolding origin of the Viséan component and postfolding nature of the Early Permian and Permo/Triassic overprints. The results confirmed that the westernmost parts of the HCM were rotated clockwise after the Early Permian. Paleomagnetic studies of this zone documented shape modifications in part of the large map-scale folds as well as some of smaller meso-scale folds. Such a tectonic overprint occurred after the Early Permian, most probably in the course of Late Variscan deformations. Further results indicate that the studied N-Strending dextral strike-slip faults were active between the Early Permian and the Permo/Triassic period. Overlying breccia that covers discordantly deformed Devonian strata was formed after the Early Permian.

Název v anglickém jazyce

Palaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland)

Popis výsledku anglicky

In Devonian carbonates of the Holy Cross Mountains (HCM) are documented the record of three individual episodes of remagnetisation. The fold test performed within map-scale folds from central part of the HCM documented early synfolding origin of the Viséan component and postfolding nature of the Early Permian and Permo/Triassic overprints. The results confirmed that the westernmost parts of the HCM were rotated clockwise after the Early Permian. Paleomagnetic studies of this zone documented shape modifications in part of the large map-scale folds as well as some of smaller meso-scale folds. Such a tectonic overprint occurred after the Early Permian, most probably in the course of Late Variscan deformations. Further results indicate that the studied N-Strending dextral strike-slip faults were active between the Early Permian and the Permo/Triassic period. Overlying breccia that covers discordantly deformed Devonian strata was formed after the Early Permian.

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

<a href="/cs/project/GAP210%2F10%2F2351" target="_blank" >GAP210/10/2351: Paleomagnetismus a geochemie vulkanických hornin: Implikace pro paleopozici a vývoj pražské pánve (sv. ordovik - sp. devon)</a><br>

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

Geological Quarterly

ISSN

1641-7291

e-ISSN

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Svazek periodika

55

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

PL - Polská republika

Počet stran výsledku

12

Strana od-do

223-234

Kód UT WoS článku

000296999800004

EID výsledku v databázi Scopus

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