Facies control of the reservoir properties distribution in the carbonate rocks of epicontinental platforms

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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.

About the authors

Assel B. Khalelova

KMG Engineering

Author for correspondence.
Email: a.khalelova@niikmg.kz
Kazakhstan, Astana

References

  1. Zhemchugova VA. Reservoir sedimentology of carbonate deposits. Moscow: EAGE; 2014. (In Russ).
  2. Zhemchugova VA. Practical application of reservoir sedimentology in modeling hydrocarbon systems. Textbook for universities. Moscow: Publishing Center of Gubkin University; 2014. (In Russ).
  3. Nikonov NI, Bogatsky VI, Martynov AV, et al., editors. Timan-Pechora sedimentation basin. Atlas of geological maps. Ukhta: Timan-Pechora Research Center; 2000. (In Russ).

Supplementary files

Supplementary Files
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1. JATS XML
2. Figure 1. Depositional model of the epicontinental platform of the Timan-North Ural region [2]

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3. Figure 2. Inter-well correlation along the I-I’ line

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4. Figure 3. The principles of facies diagnostics of the epicontinental platform deposits of the Pechora Basin in the Ovinparmian time [2, edited]

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5. Figure 4. The structure of the elementary cyclite of the Ovinparma deposits under conditions of the low input of argillaceous material

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6. Figure 5. The structure of the elementary cyclite of the Ovinparma deposits under conditions of the increased input of argillaceous material

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7. Figure 6. Shallow littoral deposits

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8. Figure 7. Deposits of the lower littoral

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9. Figure 8. Upper intertidal deposits

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10. Figure 9. Supralittoral deposits

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11. Figure 10. The model of the cyclofacial subdivision of the Ovinparma horizon deposits

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12. Figure 11. An example of the location of microcracks ion the core in the rocks of the sublittoral and lower littoral

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13. Figure 12. Examples of fractures in the sediments of the Ovinparma horizon in the core column

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14. Figure 13. Mapping extract from the petrophysical surveying plane table of well N with plotted intervals of probable fracturing

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15. Figure 14. Seismic attribute map and a map of prevailing deposition conditions in the interval of member IV

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16. Figure 15. Seismic attribute map and a map of prevailing deposition conditions in the interval of member II

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Copyright (c) 2023 Khalelova A.B.

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