Abstract
To reliably appraise shallow marine hydrocarbon reservoirs, it is important to have a quantitative understanding of the geometries of parasequences, and the spatial distribution of facies within them. This study discusses the quantification of parasequence geometries and intraparasequence facies proportions in wave-dominated, shallow marine strata exposed in large scale outcrops in the Book Cliffs, Utah. The Grassy Member of the Blackhawk Formation consists of two, wave-dominated shallow marine sequences. Sequence 1 of the Grassy Member comprises two parasequences. Analysis of the depositional architecture of Parasequence 1 and Parasequence 2 shows they have very different geometries. Parasequence 1 is an aggradational-progradational parasequence which thickens gradually basinward. In contrast, Parasequence 2 is strongly progradational and shows and abrupt thickening in a basinward direction. Although Parasequence 1 and 2 have different dipsection geometries, analysis of changes in shoreface facies proportions in both, shows they have similar trends in the overall distribution of facies from proximal to distal positions. The Book Cliffs outcrops enable a complimentary analysis of strike geometries and facies proportions to also be undertaken. This study shows that within two progradational parasequences which have different geometries, there is a degree of predictability in the overall distribution of the wave-dominated shallow marinemore » shoreface facies. This suggests that, with an understanding of the large-scale depositional architecture of wave-dominated sandstones in the subsurface, the overall changes in the proportion of shoreface facies within that system can be predicted.« less
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.