IGGCAS OpenIR  > 新生代地质与环境院重点实验室
Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at-7 Ma
Sun, Jimin1,2; Ding, Zhongli1,2; Xiao, Wenjiao1,2,3; Windley, Brian F.4
2022-03-01
Source PublicationEARTH-SCIENCE REVIEWS
ISSN0012-8252
Volume226Pages:17
AbstractThe Asian interior contains the Central Asian Orogenic Belt (CAOB, the longest accretionary orogen on Earth), the largest mid-latitude desert, and the most widespread late Cenozoic airborne dust deposits (Red Clay) in the Chinese Loess Plateau. This Quaternary loess deposit is underlain by aeolian Red Clay, which has a basal age of-7 Ma throughout most of the Loess Plateau (except for several sites with latest Oligocene age in its western margin). By integrating the most recent knowledge of the reactivation and uplift history of the CAOB and the northeastern (NE) Tibetan Plateau with the magnetostratigraphic ages of the aeolian Red Clay, we provide evidence for coeval timing between the reactivation of the CAOB-NE Tibetan Plateau and the accumulation of the Red Clay, both of which began at-7 Ma. We suggest that the reactivation of the CAOB and the NE Tibetan Plateau played an important role in the deposition of the Red Clay in the latest Miocene-Pliocene through its control of the production of vast amounts of silt-sized debris created by frost weathering and of the transportation by the enhanced strength of the northwesterly wind systems. Detrital zircon ages demonstrate that the source materials of the late Cenozoic Red Clay were mainly derived from a mixed provenance of enlarged alluvial fans coherently linked to the late Cenozoic uplift of the CAOB and the NE Tibetan Plateau. These relations provide the basis for understanding the connections between the deep Earth (lithosphere) and surface processes and their impact on the ecosystem in Asia.
KeywordCentral Asian Orogenic Belt Aeolian process Cenozoic Deep-surface coupling
DOI10.1016/j.earscirev.2022.103919
Funding OrganizationNational Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences
WOS KeywordZIRCON U-PB ; CHINESE LOESS PLATEAU ; RESOLUTION MAGNETO STRATIGRAPHY ; SYNTECTONIC GROWTH STRATA ; LATE CENOZOIC DEFORMATION ; PAST 8 MA ; TIAN-SHAN ; TIEN-SHAN ; FORELAND BASIN ; QILIAN SHAN
Language英语
Funding ProjectNational Nature Science Foundation of China[41888101] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDA20070202]
Funding OrganizationNational Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; National Nature Science Foundation of China ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences
WOS Research AreaGeology
WOS SubjectGeosciences, Multidisciplinary
WOS IDWOS:000778937800002
PublisherELSEVIER
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/105126
Collection新生代地质与环境院重点实验室
岩石圈演化国家重点实验室
Corresponding AuthorSun, Jimin
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Urumqi 830011, Peoples R China
4.Univ Leicester, Sch Geog Geol & Environm, Leicester LE1 7RH, Leics, England
First Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences
Corresponding Author AffilicationInstitute of Geology and Geophysics, Chinese Academy of Sciences
Recommended Citation
GB/T 7714
Sun, Jimin,Ding, Zhongli,Xiao, Wenjiao,et al. Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at-7 Ma[J]. EARTH-SCIENCE REVIEWS,2022,226:17.
APA Sun, Jimin,Ding, Zhongli,Xiao, Wenjiao,&Windley, Brian F..(2022).Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at-7 Ma.EARTH-SCIENCE REVIEWS,226,17.
MLA Sun, Jimin,et al."Coupling between uplift of the Central Asian Orogenic Belt-NE Tibetan Plateau and accumulation of aeolian Red Clay in the inner Asia began at-7 Ma".EARTH-SCIENCE REVIEWS 226(2022):17.
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