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About Formation and Evolution of Yardangs Activated by Late Pleistocene Tectonic Movement in Dunhuang, Gansu Province of China
This document discusses a study on the formation and evolution of yardangs in Dunhuang, China that were activated by Late Pleistocene tectonic movement. The study identified three levels of river terraces in the area through fieldwork, designated as T3, T2, and T1. Electron spin resonance and optically stimulated luminescence dating determined that the terraces began evolving at 109.0-98.5 kaBP, 72.9-66.84 kaBP, and 53.2-38.0 kaBP, providing evidence of regional neotectonic movement during these periods. The formation of yardangs was dominated by tectonic uplift initially and later mainly by wind erosion, with relatively short
Detailed Information
| Author: | ['Sayed Moursy'] |
|---|---|
| Publication Year: | 2021 |
| Pages: | 12 |
| Language: | English |
| Format: | |
| Price: | FREE |
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