Facies control of the reservoir properties distribution in the carbonate rocks of epicontinental platforms
| Dublin Core | PKP Metadata Items | Metadata for this Document | |
| 1. | Title | Title of document | Facies control of the reservoir properties distribution in the carbonate rocks of epicontinental platforms |
| 2. | Creator | Author's name, affiliation, country | Assel B. Khalelova; KMG Engineering; Kazakhstan |
| 3. | Subject | Discipline(s) | |
| 3. | Subject | Keyword(s) | facies modeling; dolomitization; fracturing; seismic facies analysis |
| 4. | Description | Abstract | Background: It is difficult to imagine the modern world without hydrocarbon raw materials. Oil and gas production is not only the basis of a powerful fuel and energy complex but also the main source of foreign exchange earnings and a leading component of the budget for many countries. Carbonate rocks strike the imagination by their diversity, but at the same time they cause many problems: they are extremely variable from the point of view of reservoirs. The main problems of productive carbonate members are heterogeneity; distribution of reservoirs in the form of lenses with different configurations and strikes as well as hydrodynamic connections between the lenses is often chaotic. All of the listed problems of carbonate reservoirs are associated with secondary processes. Aim: The project aims to assess the reservoir properties of carbonate rocks from the point of view of facies zoning on the example of Ovinparm rocks. Materials and methods: In this work, we used: rock material from 8 wells (475 m), 14 wells with hydrodynamic data and a 3D seismic cube. Results: Based on the data obtained, the principles of facies diagnostics of the epicontinental platform deposits of were developed, facies of epicontinental platforms were identified, rock material was linked to logging data, a facies model and a facies map were built, a sequence stratigraphic analysis was carried out, and the regularity of the selective nature of the manifestation of secondary processes depending on the characteristics of the conditions for the accumulation of facies of epicontinental platforms was revealed, promising zones were identified taking into account the facies zoning and the intensity of the passage of secondary processes in the study area. Conclusion: By understanding how the reservoir properties are related to carbonate depositional conditions, we can predict the most interesting zones and determine the main secondary processes leading to such improved or degraded reservoir properties. |
| 5. | Publisher | Organizing agency, location | KMG Engineering |
| 6. | Contributor | Sponsor(s) | |
| 7. | Date | (DD-MM-YYYY) | 13.04.2023 |
| 8. | Type | Status & genre | Peer-reviewed Article |
| 8. | Type | Type | Research Article |
| 9. | Format | File format | |
| 10. | Identifier | Uniform Resource Identifier | https://vestnik-ngo.kz/2707-4226/article/view/108561 |
| 10. | Identifier | Digital Object Identifier (DOI) | 10.54859/kjogi108561 |
| 10. | Identifier | Digital Object Identifier (DOI) (PDF (Rus)) | 10.54859/kjogi108561-82024 |
| 11. | Source | Title; vol., no. (year) | Kazakhstan journal for oil & gas industry; Vol 5, No 1 (2023) |
| 12. | Language | English=en | ru |
| 13. | Relation | Supp. Files |
Figure 1. Depositional model of the epicontinental platform of the Timan-North Ural region [2] (218KB) doi: 10.54859/kjogi108561-65773 Figure 2. Inter-well correlation along the I-I’ line (378KB) doi: 10.54859/kjogi108561-65774 Figure 3. The principles of facies diagnostics of the epicontinental platform deposits of the Pechora Basin in the Ovinparmian time [2, edited] (734KB) doi: 10.54859/kjogi108561-65775 Figure 4. The structure of the elementary cyclite of the Ovinparma deposits under conditions of the low input of argillaceous material (496KB) doi: 10.54859/kjogi108561-65776 Figure 5. The structure of the elementary cyclite of the Ovinparma deposits under conditions of the increased input of argillaceous material (466KB) doi: 10.54859/kjogi108561-65777 Figure 6. Shallow littoral deposits (263KB) doi: 10.54859/kjogi108561-65778 Figure 7. Deposits of the lower littoral (247KB) doi: 10.54859/kjogi108561-65779 Figure 8. Upper intertidal deposits (240KB) doi: 10.54859/kjogi108561-65780 Figure 9. Supralittoral deposits (249KB) doi: 10.54859/kjogi108561-65781 Figure 10. The model of the cyclofacial subdivision of the Ovinparma horizon deposits (485KB) doi: 10.54859/kjogi108561-65783 Figure 11. An example of the location of microcracks ion the core in the rocks of the sublittoral and lower littoral (288KB) doi: 10.54859/kjogi108561-65784 Figure 12. Examples of fractures in the sediments of the Ovinparma horizon in the core column (163KB) doi: 10.54859/kjogi108561-65785 Figure 13. Mapping extract from the petrophysical surveying plane table of well N with plotted intervals of probable fracturing (591KB) doi: 10.54859/kjogi108561-65786 Figure 14. Seismic attribute map and a map of prevailing deposition conditions in the interval of member IV (253KB) doi: 10.54859/kjogi108561-65787 Figure 15. Seismic attribute map and a map of prevailing deposition conditions in the interval of member II (209KB) doi: 10.54859/kjogi108561-65788 |
| 14. | Coverage | Geo-spatial location, chronological period, research sample (gender, age, etc.) | |
| 15. | Rights | Copyright and permissions |
Copyright (c) 2023 Khalelova A.B.![]() This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License. |
