Distant Taklimakan Desert as an Important Source of Aeolian Deposits on the Chinese Loess Plateau as Evidenced by Carbonate Minerals

scientific article published on 2 May 2019

Distant Taklimakan Desert as an Important Source of Aeolian Deposits on the Chinese Loess Plateau as Evidenced by Carbonate Minerals is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2019GeoRL..46.4854M
P356DOI10.1029/2018GL081551

P2093author name stringJun Chen
Junfeng Ji
Tong He
Lianwen Liu
Xianqiang Meng
Wancang Zhao
P2860cites workWind erosion in the Qaidam basin, central Asia: Implications for tectonics, paleoclimate, and the source of the Loess PlateauQ59794521
Tracing the provenance of fine-grained dust deposited on the central Chinese Loess PlateauQ59906991
Nd and Sr isotopic characteristics of Chinese deserts: Implications for the provenances of Asian dustQ59907000
Transport, vertical structure and radiative properties of dust events in southeast China determined from ground and space sensorsQ60012091
Provenance of loess material and formation of loess deposits on the Chinese Loess PlateauQ60142308
Diverse manifestations of the mid-Pleistocene climate transitionQ61124968
Geochemical and geomorphological evidence for the provenance of aeolian deposits in the Badain Jaran Desert, northwestern ChinaQ63170327
The contribution from distant dust sources to the atmospheric particulate matter loadings at XiAn, China during springQ83294076
Eolian cannibalism: Reworked loess and fluvial sediment as the main sources of the Chinese Loess PlateauQ106691548
Late Oligocene-early Miocene birth of the Taklimakan DesertQ28647813
Onset of Asian desertification by 22 Myr ago inferred from loess deposits in ChinaQ34118465
Late Miocene episodic lakes in the arid Tarim Basin, western ChinaQ34581088
Loess Plateau storage of Northeastern Tibetan Plateau-derived Yellow River sedimentQ36250445
Geochemistry and mineralogy of the Oligo-Miocene sediments of the Valley of Lakes, MongoliaQ36357272
Dust aerosol properties and radiative forcing observed in spring during 2001-2014 over urban Beijing, ChinaQ40369601
Astronomical and glacial forcing of East Asian summer monsoon variabilityQ57144292
New eolian red clay sequence on the western Chinese Loess Plateau linked to onset of Asian desertification about 25 Ma agoQ57145316
Provenance of cryoconite deposited on the glaciers of the Tibetan Plateau: New insights from Nd-Sr isotopic composition and size distributionQ57240018
The provenance of Taklamakan desert sandQ57603819
Genetic linkage between the Yellow River, the Mu Us desert and the Chinese Loess PlateauQ57603883
Uranium isotopic constraints on the provenance of dust on the Chinese Loess PlateauQ57967664
Erg deposition and development of the ancestral Taklimakan Desert (western China) between 12.2 and 7.0 MaQ57967995
Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implicationsQ58082522
Natural and anthropogenic sources of East Asian dustQ58159924
Magnetic and geochemical characteristics of Gobi Desert surface sediments: Implications for provenance of the Chinese Loess PlateauQ58160367
Mineralogical evidence of reduced East Asian summer monsoon rainfall on the Chinese loess plateau during the early Pleistocene interglacialsQ58450618
P433issue9
P921main subjectLoess PlateauQ293730
P1104number of pages9
P304page(s)4854-4862
P577publication date2019-05-02
P1433published inGeophysical Research LettersQ5535576
P1476titleDistant Taklimakan Desert as an Important Source of Aeolian Deposits on the Chinese Loess Plateau as Evidenced by Carbonate Minerals
P478volume46

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