Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparison to the deposits of an adjacent compound bar
The depositional stratigraphy of within-channel deposits in sandy braided rivers is dominated by a variety of barforms (both singular 'unit' bars and complex 'compound' bars), as well as the infill of individual channels (herein termed 'channel fills'). The deposits of...
| Main Authors: | , , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
2011-12.
|
| Subjects: | |
| Online Access: | Get fulltext |