Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan

The article highlights the problem of oil bearing of the Domanic Formation on the territory of the Republic of Tatarstan. Comparing the geochemical characteristics of bitumen of the Semilukskian horizon and oils of the Eifelian-Frasnian terrigenous complex, it was concluded that in the Semilukskian...

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Main Authors: I.N. Plotnikova, S.B. Ostroukhov, A.A. Laptev, I.G. Gazizov, V.V. Emelyanov, N.V. Pronin4, F.F. Nosova, A.D. Salikhov
Format: Article
Language:English
Published: Georesursy Ltd. 2017-11-01
Series:Georesursy
Subjects:
Online Access:https://geors.ru/archive/article/896/
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spelling doaj-27a390b1d4524c04bc225e566723aba72020-11-25T00:38:38ZengGeoresursy Ltd.Georesursy1608-50431608-50782017-11-0119434835510.18599/grs.19.4.7Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in TatarstanI.N. Plotnikova0S.B. Ostroukhov1A.A. Laptev2I.G. Gazizov3V.V. Emelyanov4N.V. Pronin4, F.F. Nosova5V.V. Emelyanov6A.D. Salikhov7Academy of Sciences of the Republic of TatarstanVolgogradNIPImorneft Branch of LUKOIL-Engineering LLCOil and Gas Production Department Prikamneft Tatneft PJSCOil and Gas Production Department Prikamneft Tatneft PJSCOil and Gas Production Department Prikamneft Tatneft PJSCKazan (Volga region) Federal UniversityKazan (Volga region) Federal UniversityOil and Gas Production Department Prikamneft Tatneft PJSCThe article highlights the problem of oil bearing of the Domanic Formation on the territory of the Republic of Tatarstan. Comparing the geochemical characteristics of bitumen of the Semilukskian horizon and oils of the Eifelian-Frasnian terrigenous complex, it was concluded that in the Semilukskian horizon, mobile bitumen are present along with the syngenetic dispersed matter, which, according to gas-liquid chromatography, are identical to the oil of the underlying terrigenous deposits of the Pashian and Timanian horizons. These bitumens are migratory and reflect the process of upward vertical oil migration, which is responsible for the formation of industrial deposits in the Semilukskian, Sargaevskian, and Rechitskian horizons in those areas where the lithological features of the rocks and the development of superficial fracturing in them make it possible to create a collecting space. The rocks of the Domanic facies should be considered as accumulation or accumulation-generation system, oil deposits of which were formed due to oil systems generated in other sources. New methods of search are needed that allow us to quickly assess the content of migratory hydrocarbons and syngenetic organic matter. This is possible on the basis of a rapid study of the sludge, which will allow to assess the presence of mobile hydrocarbons and their quantity during drilling. An analysis of the spatial distribution of migratory hydrocarbons will allow localizing oil migration channels.https://geors.ru/archive/article/896/Domanic Formationorganic matterbitumenvertical oil migrationoil depositssearch methodsresources assessmentaccumulation system
collection DOAJ
language English
format Article
sources DOAJ
author I.N. Plotnikova
S.B. Ostroukhov
A.A. Laptev
I.G. Gazizov
V.V. Emelyanov
N.V. Pronin4, F.F. Nosova
V.V. Emelyanov
A.D. Salikhov
spellingShingle I.N. Plotnikova
S.B. Ostroukhov
A.A. Laptev
I.G. Gazizov
V.V. Emelyanov
N.V. Pronin4, F.F. Nosova
V.V. Emelyanov
A.D. Salikhov
Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan
Georesursy
Domanic Formation
organic matter
bitumen
vertical oil migration
oil deposits
search methods
resources assessment
accumulation system
author_facet I.N. Plotnikova
S.B. Ostroukhov
A.A. Laptev
I.G. Gazizov
V.V. Emelyanov
N.V. Pronin4, F.F. Nosova
V.V. Emelyanov
A.D. Salikhov
author_sort I.N. Plotnikova
title Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan
title_short Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan
title_full Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan
title_fullStr Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan
title_full_unstemmed Migration Aspect in the Oil-Bearing Capacity of the Domanic Formation in Tatarstan
title_sort migration aspect in the oil-bearing capacity of the domanic formation in tatarstan
publisher Georesursy Ltd.
series Georesursy
issn 1608-5043
1608-5078
publishDate 2017-11-01
description The article highlights the problem of oil bearing of the Domanic Formation on the territory of the Republic of Tatarstan. Comparing the geochemical characteristics of bitumen of the Semilukskian horizon and oils of the Eifelian-Frasnian terrigenous complex, it was concluded that in the Semilukskian horizon, mobile bitumen are present along with the syngenetic dispersed matter, which, according to gas-liquid chromatography, are identical to the oil of the underlying terrigenous deposits of the Pashian and Timanian horizons. These bitumens are migratory and reflect the process of upward vertical oil migration, which is responsible for the formation of industrial deposits in the Semilukskian, Sargaevskian, and Rechitskian horizons in those areas where the lithological features of the rocks and the development of superficial fracturing in them make it possible to create a collecting space. The rocks of the Domanic facies should be considered as accumulation or accumulation-generation system, oil deposits of which were formed due to oil systems generated in other sources. New methods of search are needed that allow us to quickly assess the content of migratory hydrocarbons and syngenetic organic matter. This is possible on the basis of a rapid study of the sludge, which will allow to assess the presence of mobile hydrocarbons and their quantity during drilling. An analysis of the spatial distribution of migratory hydrocarbons will allow localizing oil migration channels.
topic Domanic Formation
organic matter
bitumen
vertical oil migration
oil deposits
search methods
resources assessment
accumulation system
url https://geors.ru/archive/article/896/
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