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dc.contributor.author | Korolev E. | |
dc.contributor.author | Morozov V. | |
dc.contributor.author | Eskin A. | |
dc.contributor.author | Kolchugin A. | |
dc.date.accessioned | 2018-09-19T22:02:25Z | |
dc.date.available | 2018-09-19T22:02:25Z | |
dc.date.issued | 2016 | |
dc.identifier.issn | 0028-2448 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/144623 | |
dc.description.abstract | It was studied secondary dolomite reservoirs in Carboniferous oil saturated carbonate rocks from the Melekess depression and South-Tatar arch. It was revealed three morphological types of non-anticlinal dolomite traps: lenticular, one-layer, multilayer. It was found that the development of lenticular dolomite traps confined to zones of oilwater contacts, one-layer to flanks of anticlinal uplifts which connected with the migration ways of oil-water fluids (tectonic faults, erosion incisions). It was suggested the mechanism of formation dolomite reservoir due to the oxidation of hydrocarbons and upward migration of carbon dioxide deep fluids. | |
dc.relation.ispartofseries | Neftyanoe Khozyaystvo - Oil Industry | |
dc.subject | Diagenesis | |
dc.subject | Dolomite | |
dc.subject | Hydrocarbons | |
dc.subject | Oil-water contact | |
dc.subject | Reservoir | |
dc.title | Diagenetic dolomite reservoirs in carboniferous rocks of Melekess depression and South-Tatar arch | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 11 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 40 | |
dc.source.id | SCOPUS00282448-2016-11-SID84995662386 |