干旱区生态环境知识资源中心(Arid): Cosmogenic nuclides (Be-10 and Al-26) erosion rate constraints in the Badain Jaran Desert, northwest China: implications for surface erosion mechanisms and landform evolution

Arid

DOI	10.1007/s12303-018-0010-7
	Cosmogenic nuclides (Be-10 and Al-26) erosion rate constraints in the Badain Jaran Desert, northwest China: implications for surface erosion mechanisms and landform evolution
	Zhao, Tong 1,2,3; Liu, Wenjing 1,2,3,4,5; Xu, Zhifang 1,2,3; Liu, Taoze 6; Xu, Sheng 7; Cui, Lifeng 6; Shi, Chao 3
通讯作者	Liu, Wenjing
来源期刊	GEOSCIENCES JOURNAL
ISSN	1226-4806
EISSN	1598-7477
出版年	2019
卷号	23 期号:1 页码:59-68
英文摘要	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 Be-10 and Al-26 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 x 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.
英文关键词	cosmogenic nuclides Badain Jaran Desert erosion rate erosion mechanisms landform evolution
类型	Article
语种	英语
国家	Peoples R China ; USA ; Scotland
收录类别	SCI-E
WOS记录号	WOS:000455140500004
WOS关键词	IN-SITU ; SEDIMENT PRODUCTION ; DENUDATION RATES ; NAMIB DESERT ; HALF-LIFE ; LANDSCAPE ; EXPOSURE ; PLATEAU ; HISTORY ; CLIMATE
WOS类目	Geosciences, Multidisciplinary
WOS研究方向	Geology
来源机构	中国科学院地质与地球物理研究所
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/216040
作者单位	1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, 19 Beitucheng Western Rd, Beijing 100029, Peoples R China; 2.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China; 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China; 4.Penn State Univ, Earth & Environm Syst Inst, University Pk, PA 16802 USA; 5.Penn State Univ, Dept Geosci, University Pk, PA 16802 USA; 6.Chinese Acad Sci, Inst Geochem, State Key Lab Environm Geochem, Guiyang 550002, Guizhou, Peoples R China; 7.Scottish Univ Environm Res Ctr, E Kilbride G75 0QF, Lanark, Scotland
推荐引用方式 GB/T 7714	Zhao, Tong,Liu, Wenjing,Xu, Zhifang,et al. Cosmogenic nuclides (Be-10 and Al-26) erosion rate constraints in the Badain Jaran Desert, northwest China: implications for surface erosion mechanisms and landform evolution[J]. 中国科学院地质与地球物理研究所,2019,23(1):59-68.
APA	Zhao, Tong.,Liu, Wenjing.,Xu, Zhifang.,Liu, Taoze.,Xu, Sheng.,...&Shi, Chao.(2019).Cosmogenic nuclides (Be-10 and Al-26) erosion rate constraints in the Badain Jaran Desert, northwest China: implications for surface erosion mechanisms and landform evolution.GEOSCIENCES JOURNAL,23(1),59-68.
MLA	Zhao, Tong,et al."Cosmogenic nuclides (Be-10 and Al-26) erosion rate constraints in the Badain Jaran Desert, northwest China: implications for surface erosion mechanisms and landform evolution".GEOSCIENCES JOURNAL 23.1(2019):59-68.