Geodynamic aspects of hydrocarbon deposit formation in carbonate complex of lower carbon of the Dnieper-Donets basin and peculiarity of their forecasting and industrial development

Simple item page
dc.citation.epage63
dc.citation.issue1(32)
dc.citation.journalTitleГеодинаміка
dc.citation.spage49
dc.contributor.affiliationІнститут геології і геохімії горючих копалин Національної академії наук України
dc.contributor.affiliationInstitute of Geology and Geochemistry of Combustible Minerals of NAS of Ukraine
dc.contributor.authorЛазарук, Ярослав
dc.contributor.authorLazaruk, Yaroslav
dc.coverage.placenameЛьвів
dc.coverage.placenameLviv
dc.date.accessioned2023-07-03T08:11:44Z
dc.date.available2023-07-03T08:11:44Z
dc.date.created2028-02-22
dc.date.issued2028-02-22
dc.description.abstractМета досліджень – аналіз впливу геодинаміки регіону на формування колекторів вуглеводнів у карбонатній нижньовізейсько-турнейській товщі, обґрунтування пасток вуглеводнів у межах Мачусько-Тищенківської ділянки південної прибортової зони Дніпровсько-Донецької западини, завдання пошукового буріння на нафту і газ і нових ефективних методів стимуляції припливів газу до свердловин. Методика. В роботі використано стратиграфічний, літологічний, тектонічний, палеотектонічний методи вивчення геології та нафтоносності, а також метод геологічних аналогій. Результати. Досліджено газоносні карбонатні породи ранньовізейсько-турнейського віку на Мачусько-Тищенківській ділянці. За результатами порівняння з іншими нафтогазоносними регіонами доведено, що вони є куполами карбонатних платформ (уолсортськими фаціями). В межах ділянки виділено три ешелони біогермних вапняків, показано етапи їхнього формування. Визначено залежність колекторських властивостей вапняків від їхніх біофаціальних типів. Показано роль тектонічної тріщинуватості у формуванні порід-колекторів. Зазвичай тектонічні тріщини зацементовані кальцитом внаслідок дії пластових вод. Висловлено припущення про формування мікротріщинуватості у щільних вапняках внаслідок плюмтектоніки. Воно полягає у вторгненні високоенергетичних флюїдів з глибин землі, природному флюїдорозриві порід і формуванні в них неантиклінальних вуглеводневих скупчень. Ймовірними місцями прориву флюїдів можуть бути зони глибинних розломів: Мачусько-Тищенківську ділянку перетинає Інгулецько-Криворізько-Крупецька шовна зона. Заповнення мікротріщин вуглеводнями запобігає їх цементуванню. Наведено приклади мікротріщинуватості в керні свердловин. Встановлено зменшений винос керна з мікротріщинуватих пластів. Для виділення у карбонатних товщах інтервалів з мікротріщинуватістю пропонується застосовувати інформацію про зменшення винесення керна, а також швидкості буріння порід. З метою стабілізації та збільшення припливів газу з карбонатних колекторів до свердловин запропоновано застосування скерованих багатоступеневих гідророзривів, а також кислотних гідророзривів, які забезпечать зв’язок свердловин з газонасиченими колекторами. Визначено ймовірні чинники негативного впливу на довкілля під час проведення гідророзривів. Наукова новизна. На значних глибинах крім тектонічної тріщинуватості можлива адіабатична мікротріщинуватість щільних літотипів порід, зумовлена природним флюїдоророзривом осадової товщі вуглеводневими газами. Це дає можливість відкриття вуглеводневих скупчень нового типу, які не пов’язані з антиклінальними пастками. Практична значущість. Рекомендовано геофізичні дослідження та розміщення шести свердловин з метою пошуків покладів вуглеводнів на Мачусько-Тищенківській ділянці. Рекомендовано застосовувати ефективні методи збільшення припливу газу до свердловин з низькопроникних карбонатних порід.
dc.description.abstractThe purpose of the research is to analyze the impact of the region’s geodynamics on the formation of hydrocarbon reservoirs in the carbonate Lower Visean-Tournaisian stratum. The paper is focused on the substantiation of hydrocarbon traps within the Machukhy-Tyshchenky area of the southern zone of the DnieperDonets basin, as well as oil and gas exploratory drilling and new effective methods of stimulating gas inflows to boreholes. Methodology. The study applies the stratigraphic, lithological, tectonic, paleotectonic methods of studying geology and oil potential, as well as the method of geological analogies. Results. Gas-bearing carbonate rocks of the Early Visean-Tournaisian age in the Machuhy-Tyshchenky area have been studied. A comparison with other oil and gas regions has shown that they are the domes of carbonate platforms (Wаulsoгtiаn facies). Three echelons of bioherm limestones have been identified within the the area. The research helped to describe the stages of their formation and determine the dependence of reservoir properties of limestones on their biofacial types. The role of tectonic fracture in the formation of reservoir rocks is shown. As a rule, tectonic fractures are cemented by calcite under the action of formation waters. An assumption is made about the formation of microfractures in dense limestones due to the action of plumectonic. It consists in the intrusion of high-energy fluids from the depths of the earth, the natural fluid fracturing of rocks and the formation of nonanticlinal hydrocarbon accumulations in them. Probable places of fluid breakthrough may be zones of deep faults: the Ingulets-Kryvorizhzhya-Krupetsk fault zone crosses Machuhy-Tyshchenky area. Filling microfractures with hydrocarbons prevents their cementation. The paper gives examples of microfracturing in the cores of boreholes and establishes reduced core from microfracture intervals. To identify microfracturing intervals in carbonate rocks, it is proposed to use information on the reduction of core, as well as the speed drilling of rocks. The study suggests using multistage hydrofracturing and acid hydrofracturing in order to stabilize and increase gas influxes from carbonate reservoirs to the boreholes. Such technology should provide the connection between the borehole and oil-saturated reservoirs. Probable factors of negative impact on the environment during hydrofracturing have been identified. Originality. Adiabatic microfracturing of dense lithotypes of rocks is possible at considerable depths, in addition to tectonic fracturing. It is due to natural fluid fracturing of sedimentary strata by hydrocarbon gases. This gives hope for the discovery of new types of hydrocarbon deposits that are not associated with anticline traps. Practical significance. Geophysical surveys and the location of six boreholes are recommended in order to search for hydrocarbon deposits in the Machuhy-Tyshchenky area. The study suggests effective methods for increasing gas influxes to boreholes from low-permeability carbonate rocks.
dc.format.extent49-63
dc.format.pages15
dc.identifier.citationLazaruk Y. Geodynamic aspects of hydrocarbon deposit formation in carbonate complex of lower carbon of the Dnieper-Donets basin and peculiarity of their forecasting and industrial development / Yaroslav Lazaruk // Geodynamics. — Lviv : Lviv Politechnic Publishing House, 2022. — No 1(32). — P. 49–63.
dc.identifier.citationenLazaruk Y. Geodynamic aspects of hydrocarbon deposit formation in carbonate complex of lower carbon of the Dnieper-Donets basin and peculiarity of their forecasting and industrial development / Yaroslav Lazaruk // Geodynamics. — Lviv : Lviv Politechnic Publishing House, 2022. — No 1(32). — P. 49–63.
dc.identifier.doidoi.org/10.23939/jgd2022.02.049
dc.identifier.urihttps://ena.lpnu.ua/handle/ntb/59371
dc.language.isoen
dc.publisherВидавництво Львівської політехніки
dc.publisherLviv Politechnic Publishing House
dc.relation.ispartofГеодинаміка, 1(32), 2022
dc.relation.ispartofGeodynamics, 1(32), 2022
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dc.relation.referencesenbelt. Tectonic inversion of rift-like structure.
dc.relation.referencesenGeodynamics, 2(31), 53–65. (In Ukrainian).
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dc.relation.referencesenKhomyn, V. R. (2013). Features of geological
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dc.relation.referencesenGonchar, V. V. (2019). Tectonic inversion of the
dc.relation.referencesenDnieper-Donetsk basin and Donbas (models and
dc.relation.referencesenreconstructions). Geophysics. Journal, 41(5), 47–86. (In Ukrainian). https://doi.org/10.24028/gzh.0203-3100.v41i5.2019.184444
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dc.relation.referencesenin the Missisippian Lodgepole Formation of
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dc.relation.referencesenhttps://doi.org/10.3997|1365-2397.fb2022022
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dc.relation.referencesennorth-east Oklahoma. Am. Ass. Petroleum.
dc.relation.referencesenGeologists Vull., 41, 2530–2544. https://doi.org/10.1306/0BDA59BA-16BD-11D7-8645000102C1865D
dc.relation.referencesenKurovets, I., Prykhodko, O., Hrytsyk, I., Melnychuk, S.
dc.relation.referencesen(2019). Geothermal conditions of the Eastern oil
dc.relation.referencesenand gas region of Ukraine. Geology and geochemistry of combustible minerals, 179(2), 47–54.
dc.relation.referencesen(In Ukrainian). https://doi.org/10.15407/ggcm2019.02
dc.relation.referencesenLazaruk, J. G. and Kreidenkov, V. G. (2000). Lithofacial-paleogeomorphological reconstructions as a
dc.relation.referencesenbasis for forecasting oil and gas traps in carbonate
dc.relation.referencesenrocks. Geology and geochemistry of combustible
dc.relation.referencesenminerals, 1, 37–47. (In Ukrainian).
dc.relation.referencesenLazaruk, J. G. (2006). Theoretical aspects and methods
dc.relation.referencesenof searching for hydrocarbon deposits in nonanticline traps (on the example of XIIa deposits of
dc.relation.referencesenthe microfaunal horizon of the Dnieper-Donetsk
dc.relation.referencesenbasin). Kyiv: UkrDGRI, 110. (In Ukrainian).
dc.relation.referencesenLazaruk, Ya, Karabyn, V. (2020). Shale gas in
dc.relation.referencesenWestern Ukraine: perspectives, resources,
dc.relation.referencesenenviromental and the thechnogenic risk of
dc.relation.referencesenproduction. Petroleum and coal, 62(1), 836–844.
dc.relation.referencesenhttps://sci.ldubgd.edu.ua/handle/123456789/7543
dc.relation.referencesenLebid, V. P. (2016). About features of development of
dc.relation.referencesena new direction of geological prospecting works in
dc.relation.referencesenthe Eastern region of Ukraine. Article 2. Contours
dc.relation.referencesenof the deep model of oil and gas potential of the
dc.relation.referencesenbasogenic complex. Mineral resources of Ukraine, 4, 39–46. (In Ukrainian).
dc.relation.referencesenLukin, A. E. and Korzhnev, S. G. (1999). TournaisianLower Visean reef-carbonate complex of the
dc.relation.referencesenDnieper-Donetsk depression and general problems of
dc.relation.referencesenthe formation of the Early Carboniferous oil and gas
dc.relation.referencesenreefs. Geological Journal, 2, 21–32. (In Russian).
dc.relation.referencesenLukin, A. E. (2000). Injections of deep hydrocarbonpoly minerals in rocks of deep oil and gas basins:
dc.relation.referencesenthe nature, application and epistemological value.
dc.relation.referencesenGeologicheskij zhurnal, 2, 21–32 (In Russian).
dc.relation.referencesenLukin A.E. (2004). About through-formation fluidconducting systems in oil and gas basins.
dc.relation.referencesenGeological Journal, 3, 34–45 (In Russian).
dc.relation.referencesenLukin, A., Benko, V., Gladun, V., Zdorovenko, M.,
dc.relation.referencesenMezhuev, V., Ogar, V., Sergiy, G., Tsekha, O. &
dc.relation.referencesenSchukin, N. (2005). The Bogatoysko-OrelskoZatishnyansky mega-atoll is a large area of oil and
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dc.rights.holder© Інститут геології і геохімії горючих копалин Національної академії наук України, 2022
dc.rights.holder© Інститут геофізики ім. С. І. Субботіна Національної академії наук України, 2022
dc.rights.holder© Національний університет “Львівська політехніка”, 2022
dc.rights.holder© Lazaruk Yaroslav
dc.subjectплюмтектоніка
dc.subjectмікротріщинуватість
dc.subjectкарбонатний колектор
dc.subjectседиментація
dc.subjectнетрадиційні поклади вуглеводнів
dc.subjectplume tectonics
dc.subjectmicrofracturing
dc.subjectcarbonate reservoir
dc.subjectsedimentation
dc.subjectunconventional hydrocarbon deposits
dc.subject.udc553.98.2
dc.subject.udc551.24
dc.subject.udc552.5(477/7)
dc.titleGeodynamic aspects of hydrocarbon deposit formation in carbonate complex of lower carbon of the Dnieper-Donets basin and peculiarity of their forecasting and industrial development
dc.title.alternativeГеодинамічні аспекти формування родовищ вуглеводнів у карбонатних відкладах нижнього карбону Дніпровсько-Донецької западини та особливості їх прогнозування і промислового освоєння
dc.typeArticle

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