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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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/ |
work_keys_str_mv |
AT inplotnikova migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT sbostroukhov migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT aalaptev migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT iggazizov migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT vvemelyanov migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT nvpronin4ffnosova migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT vvemelyanov migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan AT adsalikhov migrationaspectintheoilbearingcapacityofthedomanicformationintatarstan |
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1725296569115213824 |