Matches in SemOpenAlex for { <https://semopenalex.org/work/W4309046984> ?p ?o ?g. }
- W4309046984 endingPage "111240" @default.
- W4309046984 startingPage "111240" @default.
- W4309046984 abstract "This paper comprehensively analyzes the geochemical, mineralogical and petrographical properties combined with bulk kinetics modeling of the Domanik organic-rich carbonate from various depth intervals in Kuzminovsky oilfield (well № 26 R), Volga-Ural Basin, Russia. The results show that, the Domanik carbonate-rich samples are characterized by high content of the total organic matter (TOC) up to 13.31 wt %, and contain mainly Type II kerogen with a slight II/III kerogen type, reaching very good to excellent oil generation potential. Moreover, the studied samples contain hydrogen-rich kerogen, which expected to generate paraffin, naphthene and aromatic (P–N-A) oil with low wax content as demonstrated by the Py-GC Pyrolysis combined with the abundance of fluorescent alginite, amorphous organic matter, and bituminite as established from investigations via microscope. The maturity indicators demonstrated that, most of the examined Domanik carbonate-rich samples, with a burial depth between 1726.5 m and 1784.9 m, have generally reached low thermal maturity stages; thus, defining an immature to moderate-mature of oil generation window. The results of the kinetic models suggested that, Domanik carbonate-rich rocks with vitrinite reflectance (VRo) values in the range of 0.60–0.71%, have reached relatively low kerogen transformation ratio in the range of 10–20%, indicating low probability oil generation. These finding are confirmed by the presence of low oil saturation index of less than 100 mg HC/g rock (19.64–69.97). In addition, the results of thin section, scanning electron microscopy (SEM) and micro-computed tomography (micro-CT) showed that the studied samples are characterized by low porosity (up to 3.29%) with a wide pores size range, including interparticle, cavities, cracks and organic matter pores. The development of these pore types and their quality in the studied samples is mainly controlled by high mineralogical brittleness (i.e., carbonate and quartz) together with the high organic matter inputs. Therefore, according to the obtained results, characteristics and observations, the Domanik Formation has a high potential for commercial oil production, which typically requires hydraulic fracturing followed by an in-situ retort, mainly by thermal methods such as steam injection and in situ combustion process." @default.
- W4309046984 created "2022-11-21" @default.
- W4309046984 creator A5005831087 @default.
- W4309046984 creator A5012723876 @default.
- W4309046984 creator A5019002975 @default.
- W4309046984 creator A5022427193 @default.
- W4309046984 creator A5023467994 @default.
- W4309046984 creator A5029716563 @default.
- W4309046984 creator A5044627607 @default.
- W4309046984 creator A5045248823 @default.
- W4309046984 creator A5056681463 @default.
- W4309046984 creator A5060159225 @default.
- W4309046984 creator A5061536522 @default.
- W4309046984 creator A5061703841 @default.
- W4309046984 creator A5073694501 @default.
- W4309046984 creator A5086362544 @default.
- W4309046984 date "2023-01-01" @default.
- W4309046984 modified "2023-10-17" @default.
- W4309046984 title "Geochemical, mineralogical and petrographical characteristics of the domanik formation from north samara region in the volga-ural basin, Russia: Implication for unconventional tight oil reservoir potential" @default.
- W4309046984 cites W1964797430 @default.
- W4309046984 cites W1972701175 @default.
- W4309046984 cites W1973662203 @default.
- W4309046984 cites W1990517856 @default.
- W4309046984 cites W1994868202 @default.
- W4309046984 cites W1996497787 @default.
- W4309046984 cites W1996949067 @default.
- W4309046984 cites W2008874249 @default.
- W4309046984 cites W2017670056 @default.
- W4309046984 cites W2018323423 @default.
- W4309046984 cites W2032273166 @default.
- W4309046984 cites W2047356466 @default.
- W4309046984 cites W2053531749 @default.
- W4309046984 cites W2058772564 @default.
- W4309046984 cites W2064965427 @default.
- W4309046984 cites W2065560444 @default.
- W4309046984 cites W2066923044 @default.
- W4309046984 cites W2088267666 @default.
- W4309046984 cites W2109062485 @default.
- W4309046984 cites W2111705365 @default.
- W4309046984 cites W2135844138 @default.
- W4309046984 cites W2147156164 @default.
- W4309046984 cites W2152917047 @default.
- W4309046984 cites W2163236950 @default.
- W4309046984 cites W2320392233 @default.
- W4309046984 cites W2343739054 @default.
- W4309046984 cites W2361376569 @default.
- W4309046984 cites W2604290560 @default.
- W4309046984 cites W2665178585 @default.
- W4309046984 cites W2747778497 @default.
- W4309046984 cites W2768806773 @default.
- W4309046984 cites W2791046686 @default.
- W4309046984 cites W2898847280 @default.
- W4309046984 cites W3021450244 @default.
- W4309046984 cites W3038949490 @default.
- W4309046984 cites W3088028170 @default.
- W4309046984 cites W3088920245 @default.
- W4309046984 cites W3114109105 @default.
- W4309046984 cites W3169247161 @default.
- W4309046984 cites W3188586788 @default.
- W4309046984 cites W4200136189 @default.
- W4309046984 cites W4200138955 @default.
- W4309046984 cites W4200149467 @default.
- W4309046984 cites W4200546510 @default.
- W4309046984 cites W4247541311 @default.
- W4309046984 doi "https://doi.org/10.1016/j.petrol.2022.111240" @default.
- W4309046984 hasPublicationYear "2023" @default.
- W4309046984 type Work @default.
- W4309046984 citedByCount "5" @default.
- W4309046984 countsByYear W43090469842023 @default.
- W4309046984 crossrefType "journal-article" @default.
- W4309046984 hasAuthorship W4309046984A5005831087 @default.
- W4309046984 hasAuthorship W4309046984A5012723876 @default.
- W4309046984 hasAuthorship W4309046984A5019002975 @default.
- W4309046984 hasAuthorship W4309046984A5022427193 @default.
- W4309046984 hasAuthorship W4309046984A5023467994 @default.
- W4309046984 hasAuthorship W4309046984A5029716563 @default.
- W4309046984 hasAuthorship W4309046984A5044627607 @default.
- W4309046984 hasAuthorship W4309046984A5045248823 @default.
- W4309046984 hasAuthorship W4309046984A5056681463 @default.
- W4309046984 hasAuthorship W4309046984A5060159225 @default.
- W4309046984 hasAuthorship W4309046984A5061536522 @default.
- W4309046984 hasAuthorship W4309046984A5061703841 @default.
- W4309046984 hasAuthorship W4309046984A5073694501 @default.
- W4309046984 hasAuthorship W4309046984A5086362544 @default.
- W4309046984 hasConcept C101433766 @default.
- W4309046984 hasConcept C109007969 @default.
- W4309046984 hasConcept C126559015 @default.
- W4309046984 hasConcept C127313418 @default.
- W4309046984 hasConcept C138496976 @default.
- W4309046984 hasConcept C151730666 @default.
- W4309046984 hasConcept C15744967 @default.
- W4309046984 hasConcept C17409809 @default.
- W4309046984 hasConcept C178790620 @default.
- W4309046984 hasConcept C185592680 @default.
- W4309046984 hasConcept C199289684 @default.
- W4309046984 hasConcept C2779002002 @default.
- W4309046984 hasConcept C2779196632 @default.
- W4309046984 hasConcept C2780191791 @default.