| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4463570 | Global and Planetary Change | 2013 | 25 Pages |
Abstract
⺠Basin-margin sediment wedge developed in Eocene Tyee Forearc Basin in two stages. ⺠Small clinoforms and sandy unconfined slope deposits characterize the early stage. ⺠The later stage is characterized by larger clinoforms with channels on the slope. ⺠The two-stage development is largely controlled by the preexisting basin-topography.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Manasij Santra, Ronald J. Steel, Cornel Olariu, Michael L. Sweet,