Arid
DOI10.3389/feart.2021.711802
Provenance of Aeolian Sediments in the Ordos Deserts and Its Implication for Weathering, Sedimentary Processes
Chen, Guoxiang; Dong, Zhibao; Li, Chao; Shi, Weikang; Shao, Tianjie; Nan, Weige; Yang, Junhuai
通讯作者Dong, ZB (corresponding author), Shaanxi Normal Univ, Sch Geog & Tourism, Xian, Peoples R China.
来源期刊FRONTIERS IN EARTH SCIENCE
EISSN2296-6463
出版年2021
卷号9
英文摘要Identifying the provenance of aeolian deposits in semi-arid zones of China is beneficial in understanding Earth's surface processes and helping to alleviate ecological stress. In this paper, we use grain-size, geochemical elements, heavy-minerals, and quartz grain morphology data to investigate the potential source of aeolian sands from the Ordos Deserts (Mu Us Sandy Land and Hobq Desert). Sedimentological, geochemical and geomorphological results indicate that significant provenance differences exist among various parts of the Mu Us Sandy Land, i.e., aeolian sediments from the southwest region are obviously distinct from other areas in the Mu Us Sandy Land but show the same external provenance with the Hobq Desert referring to the sorting, mineralogical maturity, geochemical characteristics, heavy-minerals, and quartz grain morphology. Comparing the samples from the Ordos Deserts with felsic rocks from potential sources via a serious of geochemical methods, we conclude that: 1) Aeolian sands from other regions of the Mu Us are a mixture of binary provenance, i.e., one originated from local lacustrine sediments and underlying sandstones, and another from the Alxa Plateau (AP) carried by northwesterly Asian winter monsoon. 2) The fluvial deposits denuded from the Qilian Orogenic Belt in the Northeastern Tibetan Plateau (NTP) and carried by the Yellow River are likely the initial material source for the southwest region of the Mu Us Sandy Land and the Hobq Desert. 3) The Yellow River plays a significant and critical role in sediment transport for sand seas in arid and semi-arid areas of northern China.
英文关键词sediment provenance grain size geochemical element heavy mineral quartz grain morphology Ordos Deserts
类型Article
语种英语
开放获取类型gold
收录类别SCI-E
WOS记录号WOS:000674360400001
WOS关键词GRAIN-SIZE CHARACTERISTICS ; S-TYPE GRANITES ; MU US DESERT ; CHINESE LOESS ; YELLOW-RIVER ; SAND SEA ; ISOTOPIC COMPOSITIONS ; GEOCHEMICAL EVIDENCE ; QUATERNARY DEPOSITS ; HELANSHAN COMPLEX
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
来源机构兰州大学
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/363281
作者单位[Chen, Guoxiang; Dong, Zhibao; Li, Chao; Shi, Weikang; Shao, Tianjie; Nan, Weige] Shaanxi Normal Univ, Sch Geog & Tourism, Xian, Peoples R China; [Yang, Junhuai] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou, Peoples R China
推荐引用方式
GB/T 7714
Chen, Guoxiang,Dong, Zhibao,Li, Chao,et al. Provenance of Aeolian Sediments in the Ordos Deserts and Its Implication for Weathering, Sedimentary Processes[J]. 兰州大学,2021,9.
APA Chen, Guoxiang.,Dong, Zhibao.,Li, Chao.,Shi, Weikang.,Shao, Tianjie.,...&Yang, Junhuai.(2021).Provenance of Aeolian Sediments in the Ordos Deserts and Its Implication for Weathering, Sedimentary Processes.FRONTIERS IN EARTH SCIENCE,9.
MLA Chen, Guoxiang,et al."Provenance of Aeolian Sediments in the Ordos Deserts and Its Implication for Weathering, Sedimentary Processes".FRONTIERS IN EARTH SCIENCE 9(2021).
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