Autogenic Processes and Environmental Forcings Recorded in Aeolian Stratigraphy II: Numerical Experiments
Time: May 22, 2019, 10:50 AM – 11:10 AM Location: Room 217 D
Abridged Abstract: A reduced complexity aeolian dune stratification model is developed and applied to explore the role of dune morphodynamics in the creation of synthetic sections of aeolian stratigraphy originating from three sets of environmental forcing: 1) steady wind transport capacity, 2) steady bed aggradation and variable wind transport capacity, and 3) steady wind transport capacity and bed aggradation. In each scenario, the forward motion of initial, highly disorganized dunes generates a significant record exclusively containing autogenic signals that arise from early dune growth, deformation, and merger. However, continued dune growth scours deeply, and shreds all records of early dunes. Afterward, dunes self-organize into quasi-stable groups. Forward motion of dune groups create, truncate, and amalgamate sets and co-sets of cross-strata, quickly forming a second, significantly more robust stratigraphic record, which preserves a comingling of signals sourced from ongoing autogenic processes and each scenario’s specific set of environmental forcings, the allogenic boundary conditions of the sand sea. Based on these results, reservoir models may wish to consider spatial variation in permeability due to a combination of both environmental forcing and autogenic dune processes, such as self-organization. Furthermore, in the limiting view of core and outcrop, the formation and migration of dune groups may create large-scale, low angle truncation surfaces which may be indistinguishable from truncation surfaces originating from environmental forcing, such as changes in base-level.
AAPG Technical program link
Download a PDF of our AAPG ACE 2019 presentation: Download PDF
View a pre-print of our manuscript: EarthArXiv Preprint
Download the bedform strata-formation model from Github: https://github.com/travisswanson/bedform-strata-formation-model