Wei-Li Qiu

TL;DR: In this paper, the authors investigated the residual OSL signals in modern fluvial sand and suspended-sediment samples from the middle reach of the Yellow River and found that the residual equivalent dose (D e ) is found to vary with grain size, mineralogy and the techniques used for the determination.

TL;DR: The Longwangchan Paleolithic site, situated on the Yellow River terraces in the Hukou area, Shaanxi province, China, was found in 2003e2004, and two areas (Localities 1 and 2) of the site were excavated in 2005e2008.

TL;DR: In this article, a sand layer, interpreted as a hyperconcentrated flow deposit, was found interbedded between loess on a Yellow River terrace in Hukou, Shaanxi, China.

TL;DR: Wang et al. as discussed by the authors applied optical dating techniques to a Yellow River terrace sequence in the Hequ area, Shanxi Province, China, based on field investigations, four terraces were identified.

TL;DR: In this paper, five Yellow River terraces (T1 to T5) in the Mengjin area were identified in the field, and seven loess/paleosol samples from three terraces were dated using the OSL-SAR protocol on fine-grained (4-11μm) quartz and the multiple-elevated-temperature post-IR IRSL (MET-pIRIR) procedure for coarse grained (63-90mm) K-feldspar.