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warm summer climate respectively during the MIS5e, MIS5c and MIS5a periods; CEM3 represents the environment during the MIS5d and MIS5b periods with intensified winter monsoon and relatively cold climate; while the CEM4 represents the extremely strong winter monsoon environment during the MIS4 ...
The Xiashu loess is a typical Quaternary eolian deposit in southern China and represents an important terrestrial paleoclimate archive in this low-latitude monsoon region. However, the chronological framework of Xiashu loess deposition has yet to be established. Determining the timing of the onset of ...
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Liu T (1985) Loess and the environment. China Ocean Press 1985:1–481 (In Chinese) Google Scholar Liu P, Li Z, Hoey T, Kincal C, Zhang J, Zeng Q, Muller J (2013) Using advanced InSAR time series techniques to monitoring landslide movements in Badong of the Three Gorges region, Ch...
MOST studies of Quaternary climates conducted during the past 150 years have focused on glacial sequences, and for the past 25 years marine sediments have provided significant further understanding of glacial and interglacial palaeoclimates. An important
Well-distributed eolian red clay in a wide area of northern China is believed to imply the onset of an ancient East Asian monsoon system since Late Miocene. Two continuous red clay sequences spanning the time interval 7–2.6 Ma and 11–2.6 Ma in the Chin