Abstract
Sediments in the interdune area were deposited over a period from at least 43 ka to 9 ka and include several depositional cycles. The lower parts of the linear dunes were formed 6-10 ka and the dune flanks have been stabilized since then. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 69-74 |
| Number of pages | 6 |
| Journal | Unknown Journal |
| State | Published - 1 Jan 1993 |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences