Optical dating of the Yellow River terraces in the Mengjin area (China): First results

被引:15
|
作者
Meng, Yong-Min [1 ]
Zhang, Jia-Fu [1 ]
Qiu, Wei-Li [2 ]
Fu, Xiao [1 ,4 ]
Guo, Yu-Jie [1 ,3 ]
Zhou, Li-Ping [1 ]
机构
[1] Peking Univ, MOE Lab Earth Surface Proc, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
[2] Beijing Normal Univ, Sch Geog, Beijing 100875, Peoples R China
[3] Univ Wollongong, Ctr Archaeol Sci, Sch Earth & Environm Sci, Wollongong, NSW 2552, Australia
[4] Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
基金
中国国家自然科学基金;
关键词
Optical dating; K-feldspar MET-pIRIR procedure; Quartz OSL-SAR protocol; Preheat temperature; Stimulation temperature; Yellow river terrace; Mengjin area; MET-PIRIR SIGNALS; STIMULATED LUMINESCENCE; K-FELDSPAR; HUKOU AREA; LOESS; EVOLUTION; SEDIMENTS; PROTOCOL; LUOCHUAN; SEQUENCE;
D O I
10.1016/j.quageo.2015.03.006
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The chronology of the Yellow River terrace sequences is crucial for understanding its geomorphological evolution. In this study, five Yellow River terraces (T1 to T5) in the Mengjin area were identified in the field, and seven loess/paleosol samples from three terraces (T2, T4 and T5) were dated using the OSL-SAR protocol on fine grained (4-11 mu m) quartz and the multiple elevated temperature post-IR IRSL (MET-pIRIR) procedure for coarse grained (63-90 mu m) K feldspar. The results show that the quartz OSL ages were underestimated despite the good performance of the SAR protocol for quartz. The preheat and stimulation temperatures play an important role in estimating D-e values when the MET-pIRIR procedure is applied. The pIRIR D-e values obtained at higher stimulation temperatures such as 250 and 290 degrees C for our samples are considered relatively reliable, although the higher temperature pIRIR signals saturate at relatively lower dose. We recommend that the preheat and dose recovery tests should be carried out when using the MET pIRIR procedure. The 12, T4 and T5 terraces were estimated to be 176 +/- 19, >400 and >550 ka, respectively, implying that the cut through time of the Yellow River around the Sanmen Gorges is earlier than 550 ka. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:219 / 225
页数:7
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