Mississippian Meramec lithologies and petrophysical property variability, stack trend, Anadarko Basin, Oklahoma
| Autor: | Matthew J. Pranter, Deepak Devegowda, James Packwood, Carl H. Sondergeld, Ishank Gupta, Michael J. Miller, Chris T. McLain, Chandra Rai, Richard E. Larese, Kurt J. Marfurt |
|---|---|
| Rok vydání: | 2021 |
| Předmět: |
geography
geography.geographical_feature_category biology Lithology Petrophysics Stack (geology) 0211 other engineering and technologies Geochemistry Geology 02 engineering and technology Structural basin 010502 geochemistry & geophysics biology.organism_classification 01 natural sciences Geophysics Reservoir modeling Kingfisher Sequence stratigraphy 021108 energy 0105 earth and related environmental sciences |
| Zdroj: | Interpretation. 9:SE1-SE21 |
| ISSN: | 2324-8866 2324-8858 |
| DOI: | 10.1190/int-2020-0161.1 |
| Popis: | Mississippian Meramec reservoirs of the Sooner Trend in the Anadarko (Basin) in Canadian and Kingfisher Counties (STACK) play are comprised of silty limestones, calcareous siltstones, argillaceous calcareous siltstones, argillaceous siltstones, and mudstones. We found that core-defined reservoir lithologies are related to petrophysics-based rock types derived from porosity-permeability relationships using a flow-zone indicator approach. We classified lithologies and rock types in noncored wells using an artificial neural network (ANN) with overall accuracies of 93% and 70%, respectively. We observed that mudstone-rich rock type 1 exhibits high clay and relatively low calcite, whereas calcareous-rich rock type 3 has high calcite and low clay content with rock type 2 falling in between as a balance between rock types 1 and 3. Results of the ANN were applied to a suite of well logs in noncored wells in which we generated lithology and rock-type logs for the Meramec. We identified that the Meramec consists of seven stratigraphic units characterized as strike-elongate, shoaling-upward parasequences; each parasequence is capped by a marine-flooding surface. The lower three parasequences (lower Meramec) form a retrogradational parasequence set that back steps to the northwest and is capped by a maximum flooding surface. The upper Meramec is characterized by parasequences that form an aggradational to progradational stacking pattern followed again by a retrogradational trend. We predict that the parasequence stacking, associated lithology distribution, and diagenetic cements appear to control the spatial distribution of petrophysical properties (porosity, permeability, and water saturation), pore volume, and hydrocarbon pore volume (HCPV). Calcareous-rich lithologies exhibit lower porosity, permeability, HCPV, and higher water saturation. We deduced that argillaceous-rich lithologies that occur near the maximum flooding surface are the most favorable reservoir intervals because they exhibit relatively higher porosity, permeability, HCPV, and lower water saturation. Productivity could not be directly correlated to rock types as operational and completion factors as well as overpressure and oil phase play important roles on production. |
| Databáze: | OpenAIRE |
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