Facies Architecture of the Fluvial-Aeolian Buchan Formation (Upper Devonian) and Its Implications on Field Exploration: A Case Study from Ardmore Field, Central North Sea, UK

Abstract

The Upper Devonian Buchan Formation in the Central North Sea is a typical terrestrial deposit and predominantly comprises fine to medium-grained sandstones with occasional conglomerates and mudstones. The Buchan Formation has been previously described as being made up mostly of braided fluvial sandstones; however, this study confirms the presence and significance of aeolian sandstones within this fluvial-dominated sequence. Facies architecture is investigated through analogue outcrop study, well log curves and numerical facies modelling, and the results show contrasting differences between fluvial and aeolian facies. The fluvial facies is composed of multiple superimposed and sand-dominated fining-upward cycles in the vertical direction, and laterally an individual cycle has a large width/thickness ratio but is smaller than the field scale. However, the high channel deposition proportion (CDP, average value = 72%) in fluvial-dominated intervals means that it is likely all the sand bodies are interconnected. Aeolian facies comprise superimposed dune and interdune depositions and can be laterally correlated over considerable distances (over 1 km). Although the aeolian sandstones are volumetrically minor (approx. 30%) within the whole Buchan Formation, they have very high porosity and permeability (14.1% -28%, 27 -5290 mD) and therefore are excellent potential reservoirs. The fluvial sandstones are significantly cemented by quartz overgrowth and dolomite and by comparison with the aeolian sandstones are poor reservoirs. Aeolian sandstones can be differentiated from fluvial sandstones using several features: pin-stripe lamentation, good sorting, high visible porosity, friable nature and lack of muddy or conglomeratic contents; these characteristics allow aeolian sandstones can be tentatively recognized by low gamma ray values, high sonic transit time and low density

Diagenetic and geochemical studies of the Buchan Formation (Upper Devonian) in the Central North Sea

“…2) (Tang et al 2017). The overall known units comprise a fluvial (B04)-aeolian (B07 and B08)-fluvial (B09, B10 and B11) variation and generally represent a progradation-retreat-progradation cycle of the alluvial fan-based braided system with aeolian deposits occurring mainly between two main progradation periods (Tang et al 2017). The total thickness of Buchan Formation is nowhere fully penetrated, but based on seismic interpretation we estimate it to be up to 800 m.…”

“…We are uncertain about the depositional facies for sandstones in stratigraphic units B01, B02, B03, B05 and B06 due to the poor core coverage; while the units B04, B09, B10 and B11 are dominated by fluvial-braided deposits, and units B07, B08 and some minor portions in B09 and B10 contain significant aeolian deposits ( Fig. 2) (Tang et al 2017). The overall known units comprise a fluvial (B04)-aeolian (B07 and B08)-fluvial (B09, B10 and B11) variation and generally represent a progradation-retreat-progradation cycle of the alluvial fan-based braided system with aeolian deposits occurring mainly between two main progradation periods (Tang et al 2017).…”