Application of sequence stratigraphic concepts to the Upper Cretaceous Tununk Shale Member of the Mancos Shale Formation, south‐central Utah: Parasequence styles in shelfal mudstone strata

• Published in: Sedimentology 2020-01, Vol.67 (1), p.118-151
• Main Authors: Li, Zhiyang, Schieber, Juergen, Ghinassi, Massimiliano
• Format: Article
• Language: English
• Subjects: Bioturbation; Coarsening; Cretaceous; Eustatic changes; Flooding; Geological time; Heterogeneity; Identification; Laminates; Mudstone; Mudstone facies; mudstone petrography; Resolution; Sedimentary environments; Sedimentary facies; Sedimentary rocks; Sedimentary structures; sequence stratigraphy; Sequences; Sequencing; Shale; Shale gas; Shales; Storms; storm‐dominated shelf; Stratigraphy; Thickness; Tununk Shale; Turonian; Variability; Western Interior Seaway
• ISSN: 0037-0746; 1365-3091
• DOI: 10.1111/sed.12637

Although sequence stratigraphic concepts have been applied extensively to coarse‐grained siliciclastic deposits in nearshore environments, high‐resolution sequence stratigraphic analysis has not been widely applied to mudstone‐dominated sedimentary successions deposited in more distal hemipelagic to pelagic settings. To examine how sequence stratigraphic frameworks can be derived from the facies variability of mudstone‐dominated successions, the Tununk Shale Member of the Mancos Shale Formation in south‐central Utah (USA) was examined in detail through a combination of sedimentological, stratigraphic and petrographic methods. The Tununk Shale accumulated on a storm‐dominated shelf during the second‐order Greenhorn sea‐level cycle. During this eustatic event, the depositional environment of the Tununk Shale shifted laterally from distal middle shelf to outer shelf, then from an outer shelf to an inner shelf environment. At least 49 parasequences can be identified within the Tununk Shale. Each parasequence shows a coarsening‐upward trend via upward increases in silt and sand content, thickness and lateral continuity of laminae/beds, and abundance of storm‐generated sedimentary structures. Variations in bioturbation styles within parasequences are complex, although abrupt changes in bioturbation intensity or diversity commonly occur across parasequence boundaries (i.e. flooding surfaces). Due to changes in depositional environments, dominant sediment supply and bioturbation characteristics, parasequence styles in the Tununk Shale show considerable variability. Based on parasequence stacking patterns, eleven system tracts, four depositional sequences and key sequence stratigraphic surfaces can be identified. The high‐resolution sequence stratigraphic framework of the Tununk Shale reveals a hierarchy of stratal cyclicity. Application of sequence stratigraphic concepts to this thick mudstone‐dominated succession provides important insights into the underlying causes of heterogeneity in these rocks over multiple thickness scales (millimetre‐scale to metre‐scale). The detailed sedimentological characterization of parasequences, system tracts and depositional sequences in the Tununk Shale provides conceptual approaches that can aid the development of high‐resolution sequence stratigraphic frameworks in other ancient shelf mudstone successions.