Cosmogenic nuclides (10Be and 26Al) erosion rate constraints in the Badain Jaran Desert, northwest China: implications for surface erosion mechanisms and landform evolution

Both tectonics and climate affect surface erosion and change the landform. Long-term surface erosion rates determined by in situ produced cosmogenic nuclides are useful quantitative constraints for landform evolution in geological time scale. Measurements of cosmogenic 10 Be and 26 Al in the graniti...

Full description

Saved in:
Bibliographic Details
Published in:Geosciences journal (Seoul, Korea) Vol. 23; no. 1; pp. 59 - 68
Main Authors: Zhao, Tong, Liu, Wenjing, Xu, Zhifang, Liu, Taoze, Xu, Sheng, Cui, Lifeng, Shi, Chao
Format: Journal Article
Language:English
Published: Seoul The Geological Society of Korea 01-02-2019
Springer Nature B.V
한국지질과학협의회
Subjects:
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Both tectonics and climate affect surface erosion and change the landform. Long-term surface erosion rates determined by in situ produced cosmogenic nuclides are useful quantitative constraints for landform evolution in geological time scale. Measurements of cosmogenic 10 Be and 26 Al in the granitic rocks exposed in the Badain Jaran Desert, give a mean erosion rate of 7.3 ± 2.6 m/Ma, which is an order of magnitude higher than those reported in other extremely arid regions. Tectonic activity is supposed to be the first order control on regional erosion rate by comparing the 10Be erosion rates of arid regions with different precipitation ranges and tectonic activities worldwide. However the higher erosion rates in the Badain Jaran Desert compared with other arid regions within the stable tectonic background were attributed to the wind erosion and periodically warmer and wetter climate since late Pleistocene. Besides, the estimated eroded mass flux of 7.8 × 10 4 t/y suggests that erosion products of bedrocks in the Badian Jaran Desert only contribute minor desert deposits, which indicates massive exogenous materials input to the desert.
ISSN:1226-4806
1598-7477
DOI:10.1007/s12303-018-0010-7