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Title: Depositional environment, diagenetic history, and reservoir geology of the Santiago member sandstones of the Pojuca Formation (Lower Cretaceous) in the Aracas oil field, Reconcavo basin, Brazil

Thesis/Dissertation ·
OSTI ID:5968776

Core analysis, sand isolith maps, shape of SP curves, and comparison with recent depositional models defined crevasse mouth bar, distal bar, bay fill, and transitional (distal bar/bay) environments. The best potential reservoirs occur in crevasse mouth bar deposits. Ten microfacies were defined, namely, two wackes, six arenites which are the most frequent in all sandstone bodies (S-1 to S-5), and two carbonates. The diagenetic evolution of the various microfacies of the Santiago sandstone is very similar and comprises: destruction of primary porosity by compaction and burial cementation; development of secondary porosity by leaching of cements; decrease in secondary porosity by late cementation and compaction; and preservation of secondary porosity due to oil migration which halted further diagenetic evolution. Framework grains, cements, and porosity in the S-2, S-3, and S-4 reservoirs display different distribution patterns. Framework grains display patterns similar to those of depositional environment whereas cements and porosity patterns reflect predominantly diagenetic processes. They show closed geometry indicating the effect of a dome-like structure of compaction origin which probably controlled the circulation of pore fluids. Highest values of porosity occur in the least cemented areas with exception of the matrix-rich interval (S-4) where the reverse values of porosity and cement are not observed. The distribution pattern of permeability is complex, and does not follow that of porosity. It does not seem to be directly related to any observable variation in framework grains or cements.

Research Organization:
Illinois Univ., Urbana (USA)
OSTI ID:
5968776
Resource Relation:
Other Information: Thesis (Ph. D.)
Country of Publication:
United States
Language:
English