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- W2349972274 abstract "Synthetic analyses of grain size,susceptibility and oxide of Shuangyantang profile in Daning valley,the Three Gorges of the Yangtze River reveal sedimentary environment changes and eolian deposits since 3 kaBP ago in this area.There was Holocene warm humid climate in the region,but eolian deposits are formed since 3 000 a ago during the first cold period of the Holocene(1000～850 B.C.)in this area,that was the Subboreal Phase or Neoglaciation Age of the Holocene.During this stage,there were short climatic oscillations according to susceptibility and oxide research.The lower layer of the eolian deposits was primary dust accumulation in cold arid climate,but the upper loess layer was formed in cool humid climate.Strong running water transported primary eolian deposit to form secondary loess.Different water powers and weathering levels made great differences between eolian deposits in this area and those in the Yangtze River and North Loess of the Pleistocene." @default.
- W2349972274 created "2016-06-24" @default.
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- W2349972274 date "2001-01-01" @default.
- W2349972274 modified "2023-09-25" @default.
- W2349972274 title "SEDIMENTARY ENVIRONMENT AND EOLIAN DEPOSITS IN PAST 3000 a IN DANING VALLEY OF THE THREE GORGES OF THE YANGTZE RIVER" @default.
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