Publication | Open Access
An integrated petrophysical and rock physics analysis to improve reservoir characterization of Cretaceous sand intervals in Middle Indus Basin, Pakistan
57
Citations
49
References
2017
Year
Rock TestingFacies AnalysisEngineeringSeismic Reservoir CharacterizationEarth ScienceGeotechnical EngineeringBasin AnalysisSeismic StratigraphyPressure PredictionFluid SaturationMiddle Indus BasinReservoir CharacterizationGeologySedimentary PetrologyEngineering GeologySedimentologyLower Goru FormationRock PropertiesRock Physics AnalysisStructural GeologyCretaceous Sand IntervalsSand IntervalsCivil EngineeringGeomechanicsRock PhysicReservoir GeologyRock MechanicsPetrology
The sand intervals of the Lower Goru Formation of the Cretaceous age, widely distributed in the Middle and Lower Indus Basin of Pakistan, are proven reservoirs. However, in the Sawan gas field of the Middle Indus Basin, these sandstone intervals are very deep and extremely heterogeneous in character, which makes it difficult to discriminate lithologies and fluid saturation. Based on petrophysical analysis and rock physics modeling, an integrated approach is adopted to discriminate between lithologies and fluid saturation in the above-mentioned sand intervals. The seismic velocities are modeled using the Xu–White clay–sand mixing rock physics model. The calibrated rock physics model shows good consistency between measured and modeled velocities. The correlation between measured and modeled P and S wave velocities is 92.76% and 84.99%, respectively. This calibrated model has been successfully used to estimate other elastic parameters, even in those wells where both shear and sonic logs were missing. These estimated elastic parameters were cross-plotted to discriminate between the lithology and fluid content in the target zone. Cross plots clearly separate the shale, shaly sand, and gas-bearing sand clusters, which was not possible through conventional petrophysical analysis. These data clusters have been exported to the corresponding well for the purpose of interpolation between wells and to analyze the lateral and vertical variations in lithology and fluid content in the reservoir zone.
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