Search citation statements
Paper Sections
Citation Types
Year Published
Publication Types
Relationship
Authors
Journals
Carbonates in the Lower Cretaceous (Barremian to early Aptian) Kharaib Formation are reservoir rocks at giant oil fields in the UAE and Qatar. The Barremian Kharaib‐2 member (K60), the focus of this study, is in general composed of a regionally continuous succession of high‐energy, shallow‐water limestones bounded above and below by “dense” low‐energy mud‐rich strata. Despite several decades of research, conventional carbonate facies classification schemes and resulting facies groupings for the Kharaib‐2 member have failed to show a statistically acceptable correlation with core‐ and log‐derived petrophysical data. Moreover, sedimentary bodies potentially responsible for dynamic reservoir heterogeneities have not clearly been identified. This paper proposes a standardized facies classification scheme for the Kharaib‐2 carbonates based on vertical facies proportion curves (VPCs) and variogram analyses of core data to construct stratigraphic correlations at both field and regional scales. Data came from 295 cored wells penetrating the Kharaib‐2 member at ten fields in the on‐ and offshore UAE. Thin, dense intervals separating reservoir units were adopted as fourth‐order transgressive units and were used for stratigraphic correlation. Field‐scale probability maps were used to identify sedimentary bodies such as shallow‐water rudistid shoals.Regional stratigraphic correlations of the Kharaib‐2 member carbonates based on the VPCs identified variations in depositional environments, especially for the lower part of the reservoir unit; depositional facies at fields in the SE of the UAE were interpreted to be more distal compared to those at offshore fields to the NW. At a field scale, the VPCs failed to identify significant lateral variations in the carbonates. However, variogram analyses of cored wells showed spatial concentrations of specific facies in the inner ramp domain which could be correlated with high‐energy depositional bodies such as shoals dominated by rudist debris. The bodies were sinusoidal in plan view with lengths of up to 8 km and widths of ca. 1 km. Although similar‐shaped bodies with these dimensions have been reported from other carbonate depositional systems, they have not previously been reported in the Kharaib Formation. At a regional (inter‐field) scale, the stratigraphic correlation of standardized sedimentary facies remains problematic; however, mapping of facies associations and their relative proportions relative to their environments of deposition demonstrated new patterns for the stratigraphic architecture of the Kharaib‐2 member in the UAE.
Carbonates in the Lower Cretaceous (Barremian to early Aptian) Kharaib Formation are reservoir rocks at giant oil fields in the UAE and Qatar. The Barremian Kharaib‐2 member (K60), the focus of this study, is in general composed of a regionally continuous succession of high‐energy, shallow‐water limestones bounded above and below by “dense” low‐energy mud‐rich strata. Despite several decades of research, conventional carbonate facies classification schemes and resulting facies groupings for the Kharaib‐2 member have failed to show a statistically acceptable correlation with core‐ and log‐derived petrophysical data. Moreover, sedimentary bodies potentially responsible for dynamic reservoir heterogeneities have not clearly been identified. This paper proposes a standardized facies classification scheme for the Kharaib‐2 carbonates based on vertical facies proportion curves (VPCs) and variogram analyses of core data to construct stratigraphic correlations at both field and regional scales. Data came from 295 cored wells penetrating the Kharaib‐2 member at ten fields in the on‐ and offshore UAE. Thin, dense intervals separating reservoir units were adopted as fourth‐order transgressive units and were used for stratigraphic correlation. Field‐scale probability maps were used to identify sedimentary bodies such as shallow‐water rudistid shoals.Regional stratigraphic correlations of the Kharaib‐2 member carbonates based on the VPCs identified variations in depositional environments, especially for the lower part of the reservoir unit; depositional facies at fields in the SE of the UAE were interpreted to be more distal compared to those at offshore fields to the NW. At a field scale, the VPCs failed to identify significant lateral variations in the carbonates. However, variogram analyses of cored wells showed spatial concentrations of specific facies in the inner ramp domain which could be correlated with high‐energy depositional bodies such as shoals dominated by rudist debris. The bodies were sinusoidal in plan view with lengths of up to 8 km and widths of ca. 1 km. Although similar‐shaped bodies with these dimensions have been reported from other carbonate depositional systems, they have not previously been reported in the Kharaib Formation. At a regional (inter‐field) scale, the stratigraphic correlation of standardized sedimentary facies remains problematic; however, mapping of facies associations and their relative proportions relative to their environments of deposition demonstrated new patterns for the stratigraphic architecture of the Kharaib‐2 member in the UAE.
The structural evolution and timing of hydrocarbon charge potentially controls the style of diagenetic overprint and the consequent reservoir quality distribution in "Oilfield A." Tilting due to regional tectonic events may have repositioned fluid contacts and influenced the development of stylolites, cementation and microporosity development. A reconstruction of the palaeo structure of Oilfield A was undertaken in order to identify the key structural and diagenetic events, constrain their timing and tie them to seismic properties. Well picks, interpreted 3D seismic horizons and P-Impedance from the inversion of PSTM 3D seismic data were used in this study. The main reservoir from the Early Cretaceous was reconstructed by flattening on progressively shallower overburden horizons. Cross-sections dissecting the structure help to identify structural events. Published data on diagenetic events were reviewed from analogue oilfields and compared to the timing and burial depth of Reservoir 2 in Oilfield A. All key regional structural events and regional petroleum systems evolution were reconciled against the burial history of Oilfield-A. Each structural time step is compared to seismic inversion property P-impedance. Structural flattening of the Reservoir 2 seismic horizon using successively shallower overburden surfaces reveals that a structural four-way dip closure has existed in Oilfield A since the Late Cretaceous. The main closure was initially located in the north-east of the present day field with the deeper flank located to the south-west. Hydrocarbon maturity and migration, potentially from both Jurassic and Early Cretaceous sources, began in the Late Cretaceous and continued through the Tertiary. The structure was tilted towards the north during the Oligo-Miocene Zagros orogeny. At this time, the crest of the field appears to have migrated towards the north-west and the south of the field was uplifted. The palaeo free water level is likely to have been driven deeper in the north and oil may have migrated south into areas of the field previously beneath the palaeo free water level. A relationship is suggested between the position of the palaeostructural crest and low values of P-impedance from seismic inversion (P-impedance is negatively correlated to porosity). This mapping exercise supports the geological concept that oil charge was sufficiently early to have potentially prevented significant cementation on the crest of the field while flank areas became chemically compacted during burial and are consequently more heavily cemented. Structural evolution and hydrocarbon charge are rarely considered as key diagenetic inputs affecting reservoir quality distribution in carbonate reservoirs. Loosely constrained paragenetic sequences are common in reservoir characterization studies. This study uses exploration-style structural reconstruction techniques on a carbonate oilfield development. Identification of key tectonic events and detailed understanding of the timing of hydrocarbon migration into a reservoir are fundamental prior to developing a geological concept and undertaking detailed subsurface modeling of reservoir properties.
Hydrocarbon presence has been observed in flank wells much deeper than crestal wells in several onshore fields in Abu Dhabi. To explain this phenomenon the integration of paleo-structural reconstruction, petroleum system analysis, and formation evaluation was used. Thickness maps were created between the Early Cretaceous Kharaib-2 (KH-2) and several younger formations that represent paleostructure during the key tectonic and hydrocarbon expulsion events. Formation evaluation that integrates various types of logs, mud logs, geochemistry, core description and analysis have been conducted on several recent appraisal flank wells to confirm the presence of hydrocarbon below the Free Water Level (FWL).The formation evaluation, petroleum system analysis, paleo-structural reconstruction were integrated in order to understand the interesting phenomenon of paleo oil presence below the current FWL. Structural reconstructionshows that various fields have structural crestslocated in the north-east during the Lower Tertiary and remained unchanged during peak hydrocarbon migration inthe Tertiary time.South-west tilting occurred as a result of the Zagros orogeny (Miocene), such that the Lower Tertiary structural crests now lies on the flanks of the fields. As a result of this tilting,hydrocarbon remigration and redistribution occurred and in places oil was replaced by water, but traces of residual oil are still present below the current FWL.This study shows that formation fluid sampling, core and log analysis indicate that the flank wells do not have better reservoir qualities that justify a deeper contact. The study also shows that there is no observed compartmentalization that separates the flank wells with crestal area. Structural reconstruction has explained the poor reservoir properties at the field crest, where it shows that today’s crest wells were flank wells at sometime during structural evolution, and diagenesis was the major playing factor impacting rock quality.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
customersupport@researchsolutions.com
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
This site is protected by reCAPTCHA and the Google Privacy Policy and Terms of Service apply.
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.