Source potential and palynofacies of Late Jurassic “Lemeš facies”, Croatia

Laminated limestone and calcareous shale outcrop samples from the Late Jurassic “Lemeš” facies (Croatia) were investigated to characterize their organic facies and palynofacies and their hydrocarbon generative potential. The results indicate that the organic rich sediments of “Lemeš” facies were dep...

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Bibliographic Details
Published in:Organic geochemistry 2009-08, Vol.40 (8), p.833-845
Main Authors: Blažeković Smojić, Snježana, Smajlović, Jasmin, Koch, Georg, Bulić, Jeronim, Trutin, Mladen, Oreški, Ernest, Alajbeg, Anđa, Veseli, Vladimir
Format: Article
Language:English
Subjects:
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geochemistry
Hydrocarbons
Sedimentary rocks
Soil and rock geochemistry
Stratigraphy
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Summary:Laminated limestone and calcareous shale outcrop samples from the Late Jurassic “Lemeš” facies (Croatia) were investigated to characterize their organic facies and palynofacies and their hydrocarbon generative potential. The results indicate that the organic rich sediments of “Lemeš” facies were deposited within a relatively shallow marine environment at low redox potential, characterized as an oxygen depleted depositional setting with stratified bottom waters of the carbonate platform (Adriatic Carbonate Platform). The organic rich samples contain a high portion of lipid rich amorphous kerogen of algal/phytoplankton origin, enriched by bacterial biomass. Most of the analyzed samples have total organic carbon contents (TOC) greater than 3%, Rock-Eval S2 >20 mg HC/g rock, yielding Hydrogen Index (HI) values ranging from 509–602 mg HC/g TOC. According to these results, the analyzed samples have very good to excellent oil generative potential. Relatively high sulfur content suggests that the kerogen is best described as Type II-S. Biomarker maturity parameters, as well as the fluorescence of the isolated kerogen, show that the organic matter is at early to peak oil thermal maturity. The observed level of thermal maturity indicates that these samples were once buried to depths of ∼5.5–5.8 km before being uplifted in the late Tertiary. The surface outcrops of the “Lemeš” facies suggest that these strata have significant source potential and are the likely source of oil in the Croatian External Dinarides.
ISSN:0146-6380
1873-5290
DOI:10.1016/j.orggeochem.2009.05.005