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Stratigraphic significance and resolution of spectral reflectance logs in Lower Devonian carbonates of the Barrandian area, Czech Republic; a correlation with magnetic susceptibility and gamma-ray logs

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    SYSNO ASEP0342126
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleStratigraphic significance and resolution of spectral reflectance logs in Lower Devonian carbonates of the Barrandian area, Czech Republic; a correlation with magnetic susceptibility and gamma-ray logs
    Author(s) Koptíková, Leona (GLU-S) RID, SAI
    Bábek, O. (CZ)
    Hladil, Jindřich (GLU-S) RID, SAI
    Kalvoda, J. (CZ)
    Slavík, Ladislav (GLU-S) RID, SAI, ORCID
    Source TitleSedimentary geology. - : Elsevier - ISSN 0037-0738
    Roč. 225, 3/4 (2010), s. 83-98
    Number of pages16 s.
    Publication formWWW - WWW
    Languageeng - English
    CountryNL - Netherlands
    KeywordsVIS spectral reflectance ; cyclostratigraphy ; sea-level changes ; Lower Devonian ; red pelagic carbonates ; diagenesis
    Subject RIVDB - Geology ; Mineralogy
    R&D ProjectsIAAX00130702 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    GA205/08/0767 GA ČR - Czech Science Foundation (CSF)
    CEZAV0Z30130516 - GLU-S (2005-2011)
    UT WOS000277076200001
    EID SCOPUS77954596637
    DOI10.1016/j.sedgeo.2010.01.004
    AnnotationSpectral reflectance (SR) is used as a proxy for organic carbon and siliciclastic input in carbonate sediments.This study summarizes results from high-resolution outcrop SR logging of a Lower Devonian distal ramp carbonate section of the Barrandian area, Czech Republic.The SR data were correlated with parallel petrophysical and geochemical data with an aim to improving their cyclostratigraphic and event stratigraphic interpretation potential and the gaps SR data can fill. Transgressive–regressive trends, indicated by facies stacking patterns, CaCO3 data and spectral gamma-ray (GRS) logs, are well correlated in the regional context and point to third-order eustatic sea-level fluctuations.The SR data, backed up by GRS, MS and CaCO3 data indicate that the red colour in the Pragian hemipelagic limestones originated from early diagenetic hematite precipitation under the conditions of an oxygenated ocean floor and deep-sea bottom oxygenation may have been in operation during Devonian.
    WorkplaceInstitute of Geology
    ContactJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Year of Publishing2011
Number of the records: 1  

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