Controls on mud distribution and architecture along the fluvial-to-marine transition

• Published in: Geology (Boulder) 2018-11, Vol.46 (11), p.971-974
• Main Authors: van de Lageweg, Wietse I, Braat, Lisanne, Parsons, Daniel R, Kleinhans, Maarten G
• Format: Article
• Language: English
• Subjects: Architecture; Basins; clastic sediments; coastal environment; Coastal evolution; Coasts; Computer simulation; deposition; digital simulation; Distribution; Estuaries; Estuarine dynamics; estuarine environment; Estuarine environments; estuarine sedimentation; Europe; fluvial environment; Geology; Hydrodynamics; marine environment; Mathematical models; Mud; Mud flats; Naval engineering; numerical models; Numerical simulations; Organizations; Reservoirs; River flow; Rivers; Scheldt Estuary; Scheldt River; sed rocks, sediments; Sedimentary facies; Sedimentary geology; Sedimentary petrology; sedimentation; Sedimentation & deposition; Sediments; Sequence stratigraphy; Simulation; Stratigraphy; Tides; Transition zone; Western Europe
• ISSN: 0091-7613; 1943-2682
• DOI: 10.1130/G45504.1

The interaction of marine (tides and waves) and fluvial processes determines the sedimentary fill of coastal systems in the fluvial-to-marine (FTM) transition zone. Despite frequent recognition of tidal and wave influence in modern and ancient systems, our understanding of the relative importance of marine processes and their impact on mud deposition and reservoir architecture is limited. This study combined subsurface field observations and numerical simulations to investigate the relative importance of river flow, tides, waves, and mud input in governing the sedimentary fill in funnel-shaped basins along the FTM transition. Model simulations show a self-forming bar-built estuary with dynamic channels and sandy bars flanked by mud flats, which is in agreement with trends observed in nature. From three-dimensional virtual sedimentary successions, statistical tendencies for mud distribution and thickness were derived for the spectrum of marine and fluvial processes, and these values provide quantitative information on the net-to-gross ratio and mud architecture. The relative influence of marine and fluvial processes leads to a predictable facies organization and architecture, with muddier and more heterogeneous sediments toward the flanks. For the first time, our simulations allow the sedimentary fill in basins along the FTM transition to be related explicitly to hydrodynamic conditions, providing new insights into the morphosedimentary evolution of coastal systems, with implications for sequence stratigraphy.