Počet záznamů: 1  

Fine-grained non-carbonate particles embedded in neritic to pelagic limestones (Lochkovian to Emsian, Prague synform, Czech Republic): composition, provenance and links to magnetic susceptibility and gamma-ray logs

  1. 1.
    SYSNO ASEP0345504
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevFine-grained non-carbonate particles embedded in neritic to pelagic limestones (Lochkovian to Emsian, Prague synform, Czech Republic): composition, provenance and links to magnetic susceptibility and gamma-ray logs
    Tvůrce(i) Koptíková, Leona (GLU-S) RID, SAI
    Hladil, Jindřich (GLU-S) RID, SAI
    Slavík, Ladislav (GLU-S) RID, SAI, ORCID
    Čejchan, Petr (GLU-S) RID, SAI
    Bábek, O. (CZ)
    Zdroj.dok.GEOLOGICA BELGICA - ISSN 1374-8505
    Roč. 13, č. 4 (2010), s. 407-430
    Poč.str.24 s.
    Forma vydáníWWW - WWW
    Jazyk dok.eng - angličtina
    Země vyd.BE - Belgie
    Klíč. slovanon-carbonate impurities ; limestones ; magnetic susceptibility ; gamma-ray spectrometry ; REE distributions ; atmospheric dust ; Lower Devonian ; Prague Synform
    Vědní obor RIVDB - Geologie a mineralogie
    CEPIAA300130702 GA AV ČR - Akademie věd
    GAP210/10/2351 GA ČR - Grantová agentura ČR
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000285908500009
    EID SCOPUS77954615064
    AnotaceThis paper deals with the variations in non-carbonate impurities trapped in the Lower Devonian limestone beds in the Prague Synform.Different assemblages are encountered for the Lochkovian, lower Emsian and Pragian. The Lochkovian is characterized by pyrite–pyrrhotite assemblages with lower abundance of iron oxides-oxyhydroxides,the Pragian shows relatively abundant iron oxides-oxyhydroxides.Major changes in magnetic susceptibility (MS) and gamma-ray spectrometric logs also coincide with the Lochkovian/Pragian boundary. Maximum values of MS and relatively high Th, K concentrations above the boundary correspond to the elevated amounts of barite and Ba concentrations.This level is interpreted as a significant interval with elevated delivery of impurities of aeolian origin, deceleration of sedimentation rate together with decreased carbonate productivity.REE distributions are indicative of the aeolian origin of trapped impurities.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2011
Počet záznamů: 1  

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