Počet záznamů: 1  

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

  1. 1.
    SYSNO ASEP0368273
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevPalaeomagnetic age constraints on folding and faulting events in devonian carbonates of the Kielce Fold Zone southern Holy Cross Mountains, Central Poland)
    Tvůrce(i) Szaniawski, R. (PL)
    Konon, A. (PL)
    Grabowski, J. (PL)
    Schnabl, Petr (GLU-S) RID, SAI, ORCID
    Zdroj.dok.Geological Quarterly. - : Państwowy Instytut Geologiczny - ISSN 1641-7291
    Roč. 55, č. 3 (2011), s. 223-234
    Poč.str.12 s.
    Forma vydáníWWW - WWW
    Jazyk dok.eng - angličtina
    Země vyd.PL - Polsko
    Klíč. slovapaleomagnetic components ; remagnetization ; tectonics
    Vědní obor RIVDE - Zemský magnetismus, geodézie, geografie
    CEPGAP210/10/2351 GA ČR - Grantová agentura ČR
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000296999800004
    EID SCOPUS81355123033
    AnotaceIn 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-S trending 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.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2012
    Elektronická adresahttp://gq.pgi.gov.pl/gq/article/view/7602/pdf_23
Počet záznamů: 1  

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