Pregled bibliografske jedinice broj: 408160
Source potential and palynofacies of Late Jurassic "Lemeš facies", Croatia
Source potential and palynofacies of Late Jurassic "Lemeš facies", Croatia // Organic geochemistry, 40 (2009), 8; 833-845 doi:10.1016/j.orggeochem.2009.05.005 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 408160 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Source potential and palynofacies of Late Jurassic "Lemeš facies", Croatia
Autori
Blažeković Smojić, Snježana ; Smajlović, Jasmin ; Koch, Georg ; Bulić, Jeronim ; Trutin, Mladen ; Oreški, Ernest ; Alajbeg, Anđa ; Veseli, Vladimir
Izvornik
Organic geochemistry (0146-6380) 40
(2009), 8;
833-845
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
source rock; organic facies; palynofacies; biomarker geochemistry; hopanes; steranes; mono and triaromatic steroids; Lemeš facies; Late Jurassic; Adriatic Carbonate Platform; Croatia
Sažetak
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 paltform (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 content (TOC) grater than 3%, Rock-Eval S2 higher than 20 mg HC/g rock, yielding Hydrogen Index (HI) values ranging from 503 to 610 mg HC/g TOC. According to these results, the analyzed samples have very good to excellent oil-generative potential. Relatively high sulfur content suggest 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 to 5.8 km befora being uplifted in the Late Terniary. 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
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Dentalna medicina
POVEZANOST RADA
Projekti:
065-0650445-1277 - Nearomatski naftalan –istraživanje sastava i bioloških učinaka na epitelna tkiva (Alajbeg, Ivan, MZOS ) ( CroRIS)
119-1951293-1162 - Dokazi biotičkih i abiotičkih promjena u fosilnim okolišima (Sremac, Jasenka, MZOS ) ( CroRIS)
181-1811096-1093 - Osnovna geološka karta Republike Hrvatske 1:50.000 (Belak, Mirko, MZOS ) ( CroRIS)
181-1953068-0363 - Holocenski sedimenti kao zapis promjena u okolišu Jadranskih slivova (Koch, Georg, MZOS ) ( CroRIS)
195-1953068-2704 - Dinarski krš: geološka evolucija, mineralne sirovine, paleotla i tla (Durn, Goran, MZOS ) ( CroRIS)
Ustanove:
INA-Industrija nafte d.d.,
Stomatološki fakultet, Zagreb,
Prirodoslovno-matematički fakultet, Zagreb,
Geotehnički fakultet, Varaždin,
Hrvatski geološki institut,
Hrvatski prirodoslovni muzej
Profili:
Ernest Oreški
(autor)
Mladen Trutin
(autor)
Vladimir Veseli
(autor)
Anđa Alajbeg
(autor)
Georg Koch
(autor)
Jeronim Bulić
(autor)
Jasmin Smajlović
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus