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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 ASEP 0342126 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title 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 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, ORCIDSource Title Sedimentary geology. - : Elsevier - ISSN 0037-0738
Roč. 225, 3/4 (2010), s. 83-98Number of pages 16 s. Publication form WWW - WWW Language eng - English Country NL - Netherlands Keywords VIS spectral reflectance ; cyclostratigraphy ; sea-level changes ; Lower Devonian ; red pelagic carbonates ; diagenesis Subject RIV DB - Geology ; Mineralogy R&D Projects IAAX00130702 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR) GA205/08/0767 GA ČR - Czech Science Foundation (CSF) CEZ AV0Z30130516 - GLU-S (2005-2011) UT WOS 000277076200001 EID SCOPUS 77954596637 DOI 10.1016/j.sedgeo.2010.01.004 Annotation Spectral 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. Workplace Institute of Geology Contact Jana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272 Year of Publishing 2011
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