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Sealing Attributes of Giant Fields from Around the World

Jose I. Guzman1, Rod Sloan2, Shengyu Wu1, and Shaoqing Sun2
1 C&C Reservoirs, Inc, Houston, TX
2 C&C Reservoirs, Ltd, Maidenhead, Berks, United Kingdom

A systematic analysis of sealing parameters from over 220 giant fields (>500 MMBOE EUR) in 84 basins worldwide reveals that Previous HitsealNext Hit capacity, i.e., the calculated hydrocarbon column height that a Previous HitsealNext Hit can support, is more important than the degree of trap fill. The average hydrocarbon column height retained is ~1500 ft and the maximum is ~7500 ft. However, over half of the fields occur in underfilled traps. This suggests that if structural closure is sufficiently large and hydrocarbon charge is adequate, giant accumulations can occur even if the traps are leaking.

Over 33% of all reservoirs in giant fields are sealed by Previous HittopNext Hit-dominated seals that involve a combination of simple Previous HittopNext Hit seals and lateral faults, updip faults and/or lateral stratigraphic seals. Nearly 25% of the reservoirs are capped by simple Previous HittopNext Hit seals alone, that is, no other sealing mechanism is involved, and 22% are sealed by an updip Previous HitfaultNext Hit or a stratigraphic Previous HitsealNext Hit. Three quarters of the reservoirs are Previous HittopNext Hit-sealed by clastics (mostly shales), and only ~10% are sealed by evaporites. Previous HitTopNext Hit Previous HitsealNext Hit thickness varies from 10 ft to 6500 ft and averages ~700 ft, but Previous HitsealNext Hit thickness by itself is not a reliable indicator of hydrocarbon column height or of Previous HitsealNext Hit efficiency.

Giant fields sealed by updip faults usually require that Previous HitfaultTop throws be larger than reservoir thickness, and that average reservoir dips be >5°. Stratigraphic sealing is most common by onlap or by updip clastic facies changes in low-dip traps with large productive areas.