BÁBEK, Ondřej, Jindřich HLADIL, Jiří CHLACHULA a Leona KOPTÍKOVÁ. Correlation potential of spectral reflectance logs compared to gamma-ray and magnetic susceptibility. In Outcrops Revitalized: Tools, Techniques and Applications; SEPM Research Conference. Kilkee, Ireland: SEPM, Society for Sedimentary Geology, 2008, s. 8-8.
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Základní údaje
Originální název Correlation potential of spectral reflectance logs compared to gamma-ray and magnetic susceptibility
Název česky Korelační potenciál karotážních křivek spektrální odraznosti a jejich srovnání s gamakarotáží a magnetickou susceptibilitou
Autoři BÁBEK, Ondřej, Jindřich HLADIL, Jiří CHLACHULA a Leona KOPTÍKOVÁ.
Vydání Kilkee, Ireland, Outcrops Revitalized: Tools, Techniques and Applications; SEPM Research Conference, od s. 8-8, 1 s. 2008.
Nakladatel SEPM, Society for Sedimentary Geology
Další údaje
Originální jazyk angličtina
Typ výsledku Stať ve sborníku
Obor 10500 1.5. Earth and related environmental sciences
Stát vydavatele Irsko
Utajení není předmětem státního či obchodního tajemství
Organizační jednotka Přírodovědecká fakulta
Klíčová slova anglicky visible light spectral reflectance; sediment colour; stratigraphy
Štítky sediment colour, stratigraphy, visible light spectral reflectance
Příznaky Mezinárodní význam, Recenzováno
Změnil Změnil: Mgr. Petr Bureš, učo 40751. Změněno: 15. 4. 2012 20:35.
Anotace
Spectral reflectance analysis and digital image analysis make it possible to relate sediment colour to variation in organic carbon, carbonate content, magnetic susceptibility (MS) or directly to concentrations of particular minerals, implying a great potential for time series analysis and stratigraphic correlation. We examined visible light reflectance spectra from three sections with different lithology and age (Lower Devonian carbonates, recent lake deposits, Czech Republic; Upper Pleistocene loess, eastern Kazakhstan) using portable spectral photometer. The aim was to examine the potential of spectrophotometric logs to reveal important stratigraphic trends and boundaries on different scales. The reflectance data were logged in 2 to 10 cm interval and converted to CIE L*a*b* values, brightness and percent reflectance in seven colour spectral bands (violet to red). The colour data were compared to MS and spectral gamma ray (GRS) logs, background lithology and stratigraphy. Linear regression analysis reveals that the colorimetric data are uncorrelated with MS and GRS (R2 < 0.1). However, the spectrophotometric, MS and GRS logs can be subdivided into easily correlatable blocky, funnel-like and bell-like segments, symmetrical sinusoids and isolated peaks on different thickness scales. All the major stratigraphic features such as major disconformities, paleosol complexes in loess and annual lake layers can be easily discerned on the spectrophotometric logs, MS logs and to a lesser degree on the GRS logs. The results show that the spectrophotometric logs can have a strong potential for preliminary stratigraphic correlation in various lithologies although the role of particular colour activators may not be clearly known.
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