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Statements

Subject Item
n2:RIV%2F67985831%3A_____%2F10%3A00342126%21RIV11-GA0-67985831
rdf:type
n6:Vysledek skos:Concept
dcterms:description
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. 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.
dcterms: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 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
skos:prefLabel
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 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
skos:notation
RIV/67985831:_____/10:00342126!RIV11-GA0-67985831
n3:aktivita
n12:S n12:P n12:Z
n3:aktivity
P(GA205/08/0767), P(IAAX00130702), S, Z(AV0Z30130516)
n3:cisloPeriodika
3/4
n3:dodaniDat
n8:2011
n3:domaciTvurceVysledku
n4:8642702 n4:4732235 n4:4393961
n3:druhVysledku
n9:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n13:predkladatel
n3:idSjednocenehoVysledku
290261
n3:idVysledku
RIV/67985831:_____/10:00342126
n3:jazykVysledku
n18:eng
n3:klicovaSlova
VIS spectral reflectance; cyclostratigraphy; sea-level changes; Lower Devonian; red pelagic carbonates; diagenesis
n3:klicoveSlovo
n5:VIS%20spectral%20reflectance n5:sea-level%20changes n5:cyclostratigraphy n5:Lower%20Devonian n5:diagenesis n5:red%20pelagic%20carbonates
n3:kodStatuVydavatele
NL - Nizozemsko
n3:kontrolniKodProRIV
[47AF2D5DFE01]
n3:nazevZdroje
Sedimentary geology
n3:obor
n17:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
5
n3:projekt
n16:IAAX00130702 n16:GA205%2F08%2F0767
n3:rokUplatneniVysledku
n8:2010
n3:svazekPeriodika
225
n3:tvurceVysledku
Koptíková, Leona Slavík, Ladislav Hladil, Jindřich Bábek, O. Kalvoda, J.
n3:wos
000277076200001
n3:zamer
n15:AV0Z30130516
s:issn
0037-0738
s:numberOfPages
16