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 |
|