Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4685634 | Geomorphology | 2011 | 10 Pages |
Abstract
The proposed diffluence model might help explain other carbonate fluvial systems in which (1) tufas appear in areas with no permanent water supply, and (2) tufas are absent over extensive areas despite conditions favourable to their formation.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
M. Vázquez-Urbez, G. Pardo, C. Arenas, C. Sancho,