寒旱区科学（英文版）
寒旱區科學（英文版）
한한구과학（영문판）
SCIENCES IN COLD AND ARID REGIONS
2009年
5期
443-447
,共5页
Nanling Mountain Range%Dongjiang River valley%,red sandy sediment%grain-size analysis%arid environment
Layer LJ3 of Linjiang sttrigraphic section in Dongjiang River valley in the south of the Nanling Mountains is a set of red sandy sediments.Measured by thermoluminescence (TL) dating, it was found to be formed in MIS2-9,500±800 yr to 19,600±1,800 yr B.P. After analysis of the grain sizes of the 16 samples (LJ3-100 to LJ3-85) in this layer, it was discovered that (1) The contents of each grain group in different samples are similar. (2) The values of Md, Mz,σ,Sk and Kg vary from LJ3-100 to LJ3-85 in a narrow range. (3) The segments of each sample in the accumulative curves extend parallel with similar slopes. All the three aspects reveal the Aeolian characteristics of Layer LJ3.Therefore, it is thought that Layer LJ3 consists of red sandy sediments formed in MIS2 in the south of Nanling Mountain, which reflects the arid climate at that time.
