Abstract

The Upper Arab reservoir in the central Persian Gulf was examined for depositional, diagenetic, sequence stratigraphic and petrophysical features. This succession is composed of eight sedimentary facies that deposited on a carbonate ramp. Three-third-order sequences prograded across the Late Jurassic Arab Platform. This interval was complicated by multiple diagenetic phases including eogenesis and mesogenesis that strongly influenced reservoir properties. Dolomitization, dissolution, cementation and compaction are major diagenetic processes which played an essential role in increasing or decreasing reservoir quality. Four hydraulic flow units (HFU) were determined by flow zone indicator approach for evaluation of the reservoir quality. In addition to depositional features, diagenetic alterations have changed general HFUs characterizations such as porosity, permeability and pore-throat size. Likewise, via Lucia classification, HFUs of the Arab reservoir were grouped based on the integration of geological and petrophysical attributes in detail. Among diagenetic processes, dolomitization and dissolution have positive effects while cementation and stylolitization have a negative effect on HFUs characteristics in the studied reservoir. Put another way, since diagenetic alterations lead to the intensification of heterogeneity in carbonate reservoir, prediction of the relationship between pore type and pore throat size is a problematic issue. Recognition of the hydraulic flow units considered as a practical tool for grouping reservoir rocks and characterizing heterogeneity using porosity and permeability relationship. Finally, specifying of the contribution of various diagenetic imprints in each hydraulic flow unit in a sequence stratigraphic framework results in a conceptual reservoir model that could predict reservoir quality variations across the field.

Highlights

  • Carbonate reservoirs show extreme heterogeneity resulted from various parameters including depositional and postdepositional processes

  • HFU1 includes the higher reservoir quality intervals with high pore connectivity and composed of grain-dominated facies that was subjected to vuggy dissolution

  • This hydraulic flow units (HFU) is predominantly found at the late transgressive system tract (TST) and early high stand tract (HST)

Read more

Summary

Introduction

Carbonate reservoirs show extreme heterogeneity resulted from various parameters including depositional and postdepositional processes. The aims of this study include (1) recognizing the impact of diagenetic evolution on the heterogeneity of the Arab reservoir, (2) establishing a sequence stratigraphic model for distribution of diagenetic processes, (3) determination of hydraulic flow units and their relationship with the geological attributes and sequence stratigraphic framework. These could lead to a better understanding of reservoir property distribution, resulted from the heterogeneity of carbonate reservoirs. Dolomite is the main lithology in these units, and anhydrite is the prevalent lithology

Materials and methods
F1: Anhydrite
F3: Peloidal stromatolite boundstone
F5: Bioclast peloid packstone‐wackestone
F6: Peloidal oncoid bioclast packstone
F7: Ooid oncoid grainstone
F8: Oncoid bioclast intraclast grainstone
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call