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Geological Controls on Reservoir Development in a Leonardian...Carbonate Platform Reservoir...Digital Download

RI0266D

Geological Controls on Reservoir Development in a Leonardian (Lower Permian) Carbonate Platform Reservoir, Monahans Field, West Texas, by S. C. Ruppel. 58 p., 39 figs., 2 tables, 2002. doi.org/10.23867/RI0266D. Digital Version.

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RI0266D. Geological Controls on Reservoir Development in a Leonardian (Lower Permian) Carbonate Platform Reservoir, Monahans Field, West Texas, by S. C. Ruppel. 58 p., 39 figs., 2 tables, 2002. doi.org/10.23867/RI0266D. Downloadable PDF.

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About This Publication
This report combines borehole core and geophysical log study with porosity and permeability data to define patterns of facies and permeability distribution in a typical upper Clear Fork reservoir in the Permian Basin. Key findings are that permeability, but not porosity, varies markedly with facies and that spectral gamma ray logs are critical for defining facies, facies architecture, and reservoir quality.



ABSTRACT
Compared with similar reservoirs in younger (Guadalupian) San Andres and Grayburg Formations, reservoirs that developed in the Lower Permian (Leonardian) Clear Fork Group are typified by very low recovery efficiencies. Geological characterization of the Clear Fork reservoir at Monahans field demonstrates that although this situation may result partly from the innate heterogeneity of Clear Fork rocks, it can also result significantly from an overestimation of the mobile oil resource in these fields.

The Clear Fork reservoir at Monahans comprises the upper Clear Fork, Glorieta, and lower San Andres, all of which are characterized by cyclic, multiple-hierarchy, shallow-water, dolomitized carbonates. The cyclicity of these rocks is an important guide to their architecture and correlation. Reservoir development in these rocks reflects the combined influence of depositional and diagenetic controls. Although strong evidence points to selective porosity preservation caused by early diagenesis at cycle tops, petrophysical differences are nevertheless dominantly related to depositional facies. Tidal-flat deposits, for example, display high porosity but widely variable and generally low permeabilities and oil saturations. Subtidal grain-dominated rocks, on the other hand, exhibit similarly high porosity but much more favorable permeabilities and saturations. Distinction between these two facies is thus critical to accurate calculation of permeability and oil saturation and, in turn, to effective recovery of the remaining oil resource in Monahans and similar fields.

Although most wireline logs cannot be used to distinguish critical facies or define cyclicity, spectral gamma-ray logs, when calibrated to cores, provide an accurate picture of the distribution of poor-reservoir-quality, tidal-flat rocks and good-quality, subtidal rocks. At the same time they provide a fundamental basis for defining reservoir architecture by defining cycle boundaries. Both are necessary to develop an accurate picture of reservoir heterogeneity in Clear Fork reservoirs.


Keywords:  carbonates, diagenesis, hydrocarbons, Leonardian, Permian, reservoir characterization, stratigraphy

 

CONTENTS
ABSTRACT
INTRODUCTION
GEOLOGIC SETTING
METHODS
GENERAL STRATIGRAPHY
FACIES AND DEPOSITIONAL ENVIRONMENTS

             Tidal-Flat Facies

             Mud-Dominated Facies

             Grain-Dominated Facies

             General Paleoenvironmental Setting

 LEONARDIAN SEQUENCE STRATIGRAPHY AND CYCLICITY

             Sequence Stratigraphy

             Cyclicity

                         High-Frequency Cycles

                         Cycle Sets

                         Wireline-Log Definition Cyclicity

             Effects of Cyclicity and Paleotopography on Facies Distribution

RESERVOIR ARCHITECTURE

DIAGENESIS AND POROSITY DEVELOPMENT

             Porosity and Mineralogy Trends

             Isotope Geochemistry

RESERVOIR PETROPHYSICS

          Facies Relationships

          Vertical Porosity Trends

          Porosity and Permeability Interrelationships

          Model for Porosity and Permeability Development

RESERVOIR DEVELOPMENT

          Phi*h Trends

          Distribution of Original Oil Resources

DISCUSSION
CONCLUSIONS
ACKNOWLEDGMENTS
REFERENCES

 Figures
1. Map of West Texas, depicting paleogeography during the Leonardian and locations of major reservoirs developed in Lower Permian (Leonardian) rocks, including Monahans field
2. Diagram showing relative distribution of original oil in place in Permian oil reservoirs in the Permian Basin of
West Texas and New Mexico

3. Diagram depicting hydrocarbon volumetrics of Leonardian carbonate reservoirs in the Permian Basin, West Texas and New Mexico
4. Graph illustrating average current hydrocarbon recovery efficiencies for Leonardian reservoirs as compared with other carbonate reservoirs in the Permian Basin
5. Map of Monahans field area, showing structure at the top of the Glorieta Formation
6. Stratigraphic nomenclature of middle-Permian-age strata in the Permian Basin of West Texas and their relative importance as oil reservoirs
7. Type log for the Monahans Clear Fork reservoir, showing typical facies succession, stratigraphic terminology applied in this study, and position of major stratigraphic markers
8. Typical tidal-flat facies in the Leonardian, Monahans Clear Fork field
9. Typical grain-dominated subtidal facies in the Leonardian, Monahans Clear Fork field
10. Depositional model for middle Permian carbonate platform deposits in the Permian Basin
11. Sequence stratigraphic relationships of Leonardian-age strata in the Permian Basin of West Texas
12. General patterns of facies stacking in the Leonardian in the Permian Basin
13. Ideal cycle in Leonardian rocks on the Central Basin Platform of West Texas
14. Vertical facies succession in the Monahans Clear Fork reservoir succession, showing facies stacking patterns and cyclicity: Well No. 164
15. Vertical facies succession in the Monahans Clear Fork reservoir succession, showing facies stacking patterns and cyclicity: Well No. 270

16. Core photograph of subtidal cycle boundary
1
7. Typical cycle set in upper Clear Fork at Monahans field, showing facies- and cycle-stacking patterns and gamma-ray log response

18. Stacked cycle sets in the Glorieta

19. Styles of facies stacking and gamma-ray log response in upper Clear Fork cycle set

20. Map depicting the thickness of tidal-flat facies in the lower Glorieta Formation at Monahans field

21. Paleotopographic map of the Clear Fork reservoir interval at Monahans field compared with reservoir structure

22. Comparison of vertical facies successions at the base of the lower upper Clear Fork, which represents long-term transgression in paleotopographically low (Shell Sealy Smith No. 164) and high (Shell Sealy Smith No. 270) cores

23. Comparison of vertical facies successions in the upper, early, highstand. part of the upper Clear Fork in paleotopographically low (Shell Sealy Smith No .164) and high (Shell Sealy Smith No. 270) cores

24. Northwest-southeast cross section A-A’ based on cored well data. showing change in facies in the upper Clear Fork-Glorieta from tidal-flat-dominated (paleotopographically high) to subtidal, grain-dominated (paleotopographically low) facies

25. Northwest-southeast cross section B-B- based on spectral gamma-ray well log correlations

26. Vertical porosity trends in Leonardian cycle sets

27. Downward-decreasing porosity trends. indicated in cycle sets at Monahans field

28. Vertical mineralogical patterns in the Leonardian

29. Scatter plot of carbon and oxygen stable isotope values in cores from the Monahans Clear Fork reservoir

30. Plot of 6180 and 613c with depth. showing cycle-punctuated trends in isotope values

31. Histograms of porosity data from the Monahans Clear Fork reservoir grouped by facies

32. Histograms of permeability data from the Monahans Clear Fork reservoir, grouped by facies

33. Capillary-pressure data from the Monahans Clear Fork reservoir

34. Porosity-permeability relationship for upper Clear Fork subtidal rocks in the Monahans Clear Fork reservoir

35. Porosity-permeability relationship for lower San Andres subtidal rocks in the Monahans Clear Fork reservoir

36. Porosity-permeability relationship for tidal-flat rocks in the Monahans Clear Fork reservoir

37. Geologic model for the development of porosity and permeability in Leonardian rocks
38. Maps of phi*h for the Clear Fork reservoir at Monahans field
39. Cumulative prewaterflood production

 

Tables
1. Facies petrophysics
2.
Calculations of reservoir phi*h



Citation
Ruppel, S. C., 2002, Geological Controls on Reservoir Development in a Leonardian (Lower Permian) Carbonate Platform Reservoir, Monahans Field, West TexasThe University of Texas at Austin, Bureau of Economic Geology, Report of Investigations No. 266, 58 p. doi.org/10.23867/RI0266D.


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