LINKING MORPHODYNAMICS OF DELTAIC DISTRIBUTARY NETWORKS TO STRATIGRAPHIC CONNECTIVITY OF CHANNEL BODIES
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A USEFUL TOOL: EXPERIMENTAL DELTAS
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IN ORDER TO PREDICT STRATIGRAPHY WE NEED TO KNOW
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TO BUILD SYNTHETIC STRATIGRAPHY
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IMAGERY IS MORE READILY AVAILABLE THAN TOPOGRAPHIC DATA
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CHANNEL NETWORKS
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CHANNEL DEPTH
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BUILDING SYNTHETIC STRATIGRAPHY
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LARGE-SCALE STRUCTURE WELL CHARACTERIZED
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QUANTIFYING SANDBODY CONNECTIVITY
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OVERALL, THERE IS EXTREMELY HIGH CONNECTIVITY IN THIS SYSTEM
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BARRIER DIMENSIONS
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BARRIER WIDTH AFFECTS PERMEABILITY AND SOLUTE SPREADING
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CAN WE USE SURFACE INFORMATION TO PREDICT SUBSURFACE ARCHITECTURE?
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LARGE SCALE STRUCTURE CONTROLLED BY CHANNEL LOCATION
Description:
Explore the relationship between deltaic distributary morphodynamics networks and stratigraphic connectivity of channel bodies in this 57-minute talk. Discover a new method for constructing synthetic stratigraphy using surface imagery and learn how delta topset evolution constrains subsurface architecture. Examine experimental deltas as a tool for predicting stratigraphy, and investigate the importance of channel networks and depth in building synthetic models. Analyze large-scale structural characterization, quantify sandbody connectivity, and understand the impact of barrier dimensions on permeability and solute spreading. Gain insights into using surface information to predict subsurface architecture, with a focus on how channel location controls large-scale structure in deltaic environments.
Linking Deltaic Distributary Morphodynamics Networks to Stratigraphic Connectivity of Channel Bodies