Organic geochemical study of the upper layer of Aleksinac oil shale in the Dubrava block, Serbia
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2017
Authors
Gajica, Gordana
Šajnović, Aleksandra

Stojanović, Ksenija

Kostić, Aleksandar

Slipper, Ian

Antonijević, Milan D.

Nytoft, Hans Peter

Jovančićević, Branimir

Article (Published version)

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A detailed evaluation of geochemical properties of oil shale samples,from the outcrops of the Lower Miocene upper layer in the Dubrava area, Aleksinac basin, Serbia, was performed. For that purpose X-ray diffraction (XRD) analysis, Rock Eval pyrolysis, gas chromatography-mass spectrometry (GC-MS) analysis of biomarkers and conventional pyrolysis in an autoclave were used. Most of the samples have similar mineral compositions with predominance of clay and feldspar minerals. Three samples are characterised by an elevated content of carbonates, and among them one sample has a notable prevalence of this mineral group. This sample also demonstrated certain differences in biomarker distribution. In most samples organic matter (OM) consists predominantly of type I and II kerogens, showing high oil generative potential, whereas three samples, which contain type II kerogen with a certain input of type III kerogen, demonstrated potential to produce both, oil and gas. The OM of all samples is imm...ature and corresponds to the vitrinite reflectance of ca. 0.40%. Biomarker patterns along with Rock-Eval data indicated a strong contribution of aquatic organisms such as green and brown algae and bacteria with some influence of higher plants OM. The organic matter was deposited in a reducing lacustrine alkaline brackish to freshwater environment under warm climate conditions. Preservation of OM was governed by stratification of the water column rather than its height. Tectonic movements that caused the regional tilting of an investigated area and supported minor marine ingression and influx of fresh water played an important role in formation of the sediments. Conventional pyrolytic experiments confirmed that these sediments at the catagenetic stage could be a significant source of liquid hydrocarbons.
Keywords:
mineral composition / hydrocarbon potential / biomarkers / pyrolysis / Aleksinac oil shale / SerbiaSource:
Oil Shale, 2017, 34, 3, 197-218Publisher:
- Estonian Academy Publishers, Tallinn
Funding / projects:
- Geochemical investigations of sedimentary rocks - fossil fuels and environmental pollutants (RS-176006)
DOI: 10.3176/oil.2017.3.01
ISSN: 0208-189X
WoS: 000410464800001
Scopus: 2-s2.0-85031037156
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IHTMTY - JOUR AU - Gajica, Gordana AU - Šajnović, Aleksandra AU - Stojanović, Ksenija AU - Kostić, Aleksandar AU - Slipper, Ian AU - Antonijević, Milan D. AU - Nytoft, Hans Peter AU - Jovančićević, Branimir PY - 2017 UR - https://cer.ihtm.bg.ac.rs/handle/123456789/2162 AB - A detailed evaluation of geochemical properties of oil shale samples,from the outcrops of the Lower Miocene upper layer in the Dubrava area, Aleksinac basin, Serbia, was performed. For that purpose X-ray diffraction (XRD) analysis, Rock Eval pyrolysis, gas chromatography-mass spectrometry (GC-MS) analysis of biomarkers and conventional pyrolysis in an autoclave were used. Most of the samples have similar mineral compositions with predominance of clay and feldspar minerals. Three samples are characterised by an elevated content of carbonates, and among them one sample has a notable prevalence of this mineral group. This sample also demonstrated certain differences in biomarker distribution. In most samples organic matter (OM) consists predominantly of type I and II kerogens, showing high oil generative potential, whereas three samples, which contain type II kerogen with a certain input of type III kerogen, demonstrated potential to produce both, oil and gas. The OM of all samples is immature and corresponds to the vitrinite reflectance of ca. 0.40%. Biomarker patterns along with Rock-Eval data indicated a strong contribution of aquatic organisms such as green and brown algae and bacteria with some influence of higher plants OM. The organic matter was deposited in a reducing lacustrine alkaline brackish to freshwater environment under warm climate conditions. Preservation of OM was governed by stratification of the water column rather than its height. Tectonic movements that caused the regional tilting of an investigated area and supported minor marine ingression and influx of fresh water played an important role in formation of the sediments. Conventional pyrolytic experiments confirmed that these sediments at the catagenetic stage could be a significant source of liquid hydrocarbons. PB - Estonian Academy Publishers, Tallinn T2 - Oil Shale T1 - Organic geochemical study of the upper layer of Aleksinac oil shale in the Dubrava block, Serbia VL - 34 IS - 3 SP - 197 EP - 218 DO - 10.3176/oil.2017.3.01 ER -
@article{ author = "Gajica, Gordana and Šajnović, Aleksandra and Stojanović, Ksenija and Kostić, Aleksandar and Slipper, Ian and Antonijević, Milan D. and Nytoft, Hans Peter and Jovančićević, Branimir", year = "2017", abstract = "A detailed evaluation of geochemical properties of oil shale samples,from the outcrops of the Lower Miocene upper layer in the Dubrava area, Aleksinac basin, Serbia, was performed. For that purpose X-ray diffraction (XRD) analysis, Rock Eval pyrolysis, gas chromatography-mass spectrometry (GC-MS) analysis of biomarkers and conventional pyrolysis in an autoclave were used. Most of the samples have similar mineral compositions with predominance of clay and feldspar minerals. Three samples are characterised by an elevated content of carbonates, and among them one sample has a notable prevalence of this mineral group. This sample also demonstrated certain differences in biomarker distribution. In most samples organic matter (OM) consists predominantly of type I and II kerogens, showing high oil generative potential, whereas three samples, which contain type II kerogen with a certain input of type III kerogen, demonstrated potential to produce both, oil and gas. The OM of all samples is immature and corresponds to the vitrinite reflectance of ca. 0.40%. Biomarker patterns along with Rock-Eval data indicated a strong contribution of aquatic organisms such as green and brown algae and bacteria with some influence of higher plants OM. The organic matter was deposited in a reducing lacustrine alkaline brackish to freshwater environment under warm climate conditions. Preservation of OM was governed by stratification of the water column rather than its height. Tectonic movements that caused the regional tilting of an investigated area and supported minor marine ingression and influx of fresh water played an important role in formation of the sediments. Conventional pyrolytic experiments confirmed that these sediments at the catagenetic stage could be a significant source of liquid hydrocarbons.", publisher = "Estonian Academy Publishers, Tallinn", journal = "Oil Shale", title = "Organic geochemical study of the upper layer of Aleksinac oil shale in the Dubrava block, Serbia", volume = "34", number = "3", pages = "197-218", doi = "10.3176/oil.2017.3.01" }
Gajica, G., Šajnović, A., Stojanović, K., Kostić, A., Slipper, I., Antonijević, M. D., Nytoft, H. P.,& Jovančićević, B.. (2017). Organic geochemical study of the upper layer of Aleksinac oil shale in the Dubrava block, Serbia. in Oil Shale Estonian Academy Publishers, Tallinn., 34(3), 197-218. https://doi.org/10.3176/oil.2017.3.01
Gajica G, Šajnović A, Stojanović K, Kostić A, Slipper I, Antonijević MD, Nytoft HP, Jovančićević B. Organic geochemical study of the upper layer of Aleksinac oil shale in the Dubrava block, Serbia. in Oil Shale. 2017;34(3):197-218. doi:10.3176/oil.2017.3.01 .
Gajica, Gordana, Šajnović, Aleksandra, Stojanović, Ksenija, Kostić, Aleksandar, Slipper, Ian, Antonijević, Milan D., Nytoft, Hans Peter, Jovančićević, Branimir, "Organic geochemical study of the upper layer of Aleksinac oil shale in the Dubrava block, Serbia" in Oil Shale, 34, no. 3 (2017):197-218, https://doi.org/10.3176/oil.2017.3.01 . .