Author:
Hakimi Mohammed Hail,Saeed Shadi A.,Al-Muntaser Ameen A.,Varfolomeev Mikhail A.,Feoktistov Dmitriy A.,Suwaid Muneer A.,Djimasbe Richard,Rahim Afikah,Asiwaju Lanre,Yelwa Nura Abdulmumini
Abstract
AbstractThe distribution of aromatic hydrocarbon in sediments and oils is known to be affected by thermal maturity, source input and depositional conditions. Hence, the aromatic hydrocarbon fraction of four oil samples from different wells of the West Siberian Basin (central Russia) was investigated to determine the source of organic matter (OM), depositional environment and maturity of their source rocks. Biomarker ratios and parameters of aromatic compounds indicate that the studied oils were generated from clay-rich source rocks containing a mixed organic matter of marine and terrestrial origin, which were deposited in freshwater/deltaic to marine environmental settings under suboxic to relatively oxic conditions. Furthermore, the maturity-sensitive aromatic hydrocarbon parameters indicate that the source rocks are thermally mature, and in the peak to late maturity stage of the oil generation window. Oil–oil correlation results of various established aromatic biomarker proxies for organic matter origin, depositional environment and lithology suggests that the analyzed west Siberian Basin’s oils were generated from a variety of geological sources and can be grouped into two distinct oil families. The first oil family (group I) was generated from clay-rich source rock containing mixed organic matter with relatively high amounts of terrestrial plant input and deposited in a non-marine (freshwater/deltaic) environment under relatively oxic conditions, while the second oil family (group II) was derived from mixed organic matter with high marine OM input that was deposited in marine environment under suboxic conditions. The findings of the heterocyclic and polycyclic aromatics highlighted in this study can help for better understanding of the genetic ties between oils and their sources and have an impact on traditional hydrocarbon development in the Basin.
Publisher
Springer Science and Business Media LLC
Subject
General Energy,Geotechnical Engineering and Engineering Geology
Reference43 articles.
1. Afanasyev SA, Bukreeva GF, Vakulenko AS, Mosina OA (1993) Typification of the JK10 horizon sections of the Talinskoye deposit according to macro-heterogeneity character: Russian. Geol Geophys 34:36–40
2. Alexander R, Kagi RI, Rowland SJ, Sheppard PN, Chirila TV (1985) The effects of thermal maturity on distributions of dimethylnaphthalenes and trimethylnaphthalenes in some ancient sediments and petroleums. Geochim Cosmochim Acta 49:385–395
3. Alexander R, Bastow TB, Kagi RI, Singh RK (1992) Identification of 1, 2, 2, 5 tetramethyltetralin and 1, 2, 2, 5, 6-pentamethyltetralin as racemates in petroleum. J Chem Soc Chem Commun 23:1712–1714
4. Armstroff A, Wilkes H, Schwarzbauer J, Littke R, Horsfield B (2006) Aromatic hydrocarbon biomarkers in terrestrial organic matter of Devonian to Permian age. Palaeogeogr Palaeoclimatol Palaeoecol 240:253–274
5. Asahina K, Suzuki N (2018) Methylated naphthalenes as indicators for evaluating the source and source rock lithology of degraded oils. Org Geochem 124:46–62
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