EP026
Linking Surface Dynamics to Stratigraphic Architecture in Sedimentary Systems
Linking Surface Dynamics to Stratigraphic Architecture in Sedimentary Systems
Session ID#: 79569
Session Description:
The stratigraphic record is often used to interpret past surface processes, however the degree to which morphodynamics of the surface are translated into the subsurface remains an active line of research. For example, the lateral and vertical connectivity of channel sand bodies in the subsurface may be constrained by understanding the morphology and kinematics of channels, yet defining metrics to predict one from the other remains challenging.
We welcome submissions from those interested in bridging the gap between surface dynamics and the stratigraphic record to better understand how to predict one from the other, or vice versa. Contributions are encouraged from both subaerial and subaqueous systems on a variety of scales using laboratory-, theoretical-, numerical-, or field-based datasets.
Co-Sponsor(s):
- SEPM: Society for Sedimentary Geology -
Index Terms:
1824 Geomorphology: general [HYDROLOGY]
1825 Geomorphology: fluvial [HYDROLOGY]
1861 Sedimentation [HYDROLOGY]
1862 Sediment transport [HYDROLOGY]
Primary Convener: Elisabeth Steel, Queen's University, Geological Sciences and Geological Engineering, Kingston, ON, Canada
Convener: Sheila M Trampush, University of California Berkeley, Dept. of Geography, Berkeley, CA, United States
Primary Liaison: Elisabeth Steel, University of California Santa Barbara, Santa Barbara, CA, United States
See more of: Earth and Planetary Surface Processes
