【摘 要】
：
The Eastern Asian monsoon system is an important dynamic component of the earth climate system and composed of winter and summer monsoons.The coupling pattern of winter and summer monsoon in the Quate
【机 构】
：
Key Laboratory of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Acade
【出 处】
：
International Symposium on Aeolian Deposits in Earth History
论文部分内容阅读
The Eastern Asian monsoon system is an important dynamic component of the earth climate system and composed of winter and summer monsoons.The coupling pattern of winter and summer monsoon in the Quaternary is crucial for understanding global change.
其他文献
Carbon isotopic composition of bulk organic matter and biomarkers have been extensively applied in reconstructing paleovegetation on Chinese Loess Plateau(CLP),which has the thickest loess-paleosol de
Loess covers large parts of Central and Eastern European(CEE) lowlands,south of the maximal extent of the Pleistocene Fennoscandian ice sheets.Its coverage increases going eastward,and having an almos
The Northern Serbian province of Vojvodina is a lowland area encompassing the confluence of the Danube,Sava,Tisa(Tisza),Drava,Morava,Kara(s) and Tami(s) (Temes,Timi(s)) rivers,which separate several r
The East Asian Monsoon plays an essential role in driving the Chinese Loess Plateau(CLP) palaeoenvironmental changes.The cold winter monsoon bring detrital material from west and/or northwest China to
In the Central Great Plains,U.S.A.,landscape evolution since the Eocene has strongly influenced aeolian sediment supply,spatial patterns of aeolian activity,and the preservation potential of aeolian s
Analyses of statistical indices of particle size distribution are widely used in the investigations of loess-soil sequences.High-resolution sampling(usually every 5-10 cm) is very useful for their pal
Erosion processes are common phenomenon in the loess areas.Gully initiation and evolution usually result from combination of natural and anthropogenic causes.
The formation of aeolian deposits depends on the influence of climatic factors but also on non-climatic controls,such as local geomorphological setting and vegetation coverage.
Two loess sections KLA(10 m-thick) and KLB(7.2 m-thick) were selected to study the Holocene climate at 3750 and 3516 m a.s.l.on the northern slope of middle Kunlun Mountains,Northwest China.The grain-
To the east of the Chinese Loess Plateau(CLP),loess deposits with varying thickness are widely distributed on the northern piedmont zones and intermountain valleys of mountainous regions in central Sh