T231 Mudstone Facts: Deposition, Diagenesis, and Source of Basin Fluids

Tuesday, 24 October 2017
1:30 PM - 5:30 PM
Ballroom 6C

DIAGNOSING MECHANISMS OF OFFSHORE DEPOSITION IN THE CRETACEOUS WESTERN INTERIOR SEAWAY: A DEPOSITIONAL MODEL FOR THE LOWER BLUE GATE MEMBER, MANCOS SHALE, UINTA BASIN, UTAH

Paper number: T231-2
Program: Technical Sessions
Time: 1:35 PM – 1:50 PM

Authors

Abstract

Depositional models that use heterogeneity in mud-dominated successions to distinguish and diagnose environments within the offshore realm are still in their infancy, despite significant recent advances in understanding the complex and dynamic processes of mud deposition. Six cored intervals of the main body of the Mancos Shale, the lower Blue Gate Member, Uinta Basin, were examined sedimentologically, stratigraphically and geochemically in order to evaluate facies heterogeneity and diagnose depositional mechanisms. Unique sedimentological and geochemical features are used to identify three offshore environments of deposition: the prodelta, the mudbelt and the sediment-starved shelf. Prodelta deposits consist of interlaminated siltstone and sandstone (heterolithic), exhibit variable and stressed trace fossil assemblages, and display indicators of high sedimentation rates. The prodelta was dominated by river-fed hyperpycnal flow. Mudbelt deposits consist of heterolith and are characterized by higher bioturbation indices and more diverse trace fossil assemblages. Ripples, scours, truncations and normally graded laminations are abundant in prodelta and mudbelt deposits indicating dynamic current conditions. Mudbelt sediment dispersal was achieved by both combined flow above storm wave base and current-enhanced and wave-enhanced sediment gravity flows below storm wave base. Sediment-starved shelf deposits are dominantly siltstone to claystone with the highest calcite and organic content. Bioturbation is limited to absent. Sediment-starved shelf deposits were the result of a combination of shelfal currents and hypopycnal settling of sediment. Despite representing the smallest volume, sediment-starved shelf deposits are the most prospective for shale hydrocarbon resource development, due to elevated organic and carbonate content. Sediment-starved shelf deposits are found in either retrogradational to aggradational parasequence sets or early distal aggradational to progradational parasequence sets, bounding the maximum flooding surface. An improved framework classification of offshore mudstone depositional processes based on diagnostic sedimentary criteria advances our predictive ability in complex and dynamic mud-dominated environments and informs resource prospectivity.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-303691

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