Assessment of fluid contacts and compartmentalization in sandstone reservoirs using fluid inclusions: An example from the Magnus oil field, North Sea

Citation
Sa. Barclay et al., Assessment of fluid contacts and compartmentalization in sandstone reservoirs using fluid inclusions: An example from the Magnus oil field, North Sea, AAPG BULL, 84(4), 2000, pp. 489-504
Citations number
25
Categorie Soggetti
Earth Sciences
Journal title
AAPG BULLETIN-AMERICAN ASSOCIATION OF PETROLEUM GEOLOGISTS
ISSN journal
01491423 → ACNP
Volume
84
Issue
4
Year of publication
2000
Pages
489 - 504
Database
ISI
SICI code
0149-1423(200004)84:4<489:AOFCAC>2.0.ZU;2-C
Abstract
Location of an oil-water contact is crucial for estimating reserves and for designing production strategies. Identifying hydrodynamic barriers or baff les is also important for optimizing both recovery and flow rates. In some oil fields, identifying fluid contacts and barriers is not always possible using conventional wireline and formation testing methods. We have used a novel technique, fluid inclusion stratigraphy (FIS), to tack le these problems in the Upper Jurassic Magnus oil field in the North Sea. This technique involves systematic cleaning and crushing of small quantitie s of a large number of drill-cuttings or core samples followed by mass spec trometry without prior GC (gas chromatography) separation. The quantity and specific types of petroleum fluid trapped in pores in mineral grains are d etermined and the stratigraphic and spatial pattern of organic compounds co nstructed. For this case study, these data were integrated with quantitativ e mineralogical data derived from gamma-ray, density, sonic, and neutron po rosity logs, together with electrical resistivity. The conventional resistivity data resulted in ambiguity concerning the oil- water transition zone in both wells, interpreting the resistivity logs was locally hampered by vertical changes in reservoir lithology. The FIS data s uggested more complex transition zones (locally variable water saturations in the transition zone controlled by shales and dolomites) and petroleum ex tending deeper than suggested by the resistivity log (possibly due to lack of sensitivity of the latter to low petroleum saturations in water-wet rese rvoirs). The FIS data also suggested the presence of potential stratigraphi c (shale) and diagenetic (dolomite) barriers or baffles to fluid flow withi n the reservoir, illustrated by changes in abundance and composition of pet roleum-bearing inclusions.