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Geochronology and Mineral Composition of the Pleistocene Sediments in Xitaijinair Salt Lake Region, Qaidam Basin Preliminary Results
Zeng, Fangming; Xiang, Shuyuan
第一作者Zeng, Fangming
2017-08
发表期刊JOURNAL OF EARTH SCIENCE
ISSN1674-487X
卷号28期号:4页码:622-627
摘要Xitaijinair (XT) Salt Lake, located in the western Qaidam Basin, is significant for reconstructing the evolution of inland drying climate. However, the chronological and mineralogical records from this lake are rare. This study investigated the chronology (accelerator mass spectrometry (AMS) C-14 ages and optically stimulated luminescence (OSL) ages) and mineral compositions of sediment in the 240-cm-deep XT Section of the Xitaijinair Salt Lake region. The conclusions are drawn as follows: (1) Nine AMS C-14 ages, ranging between 33 and 40 cal ka BP, are obviously younger than the two OSL ages (57.9 and 69.1 ka). The C-14 ages probably reflect contamination with modern carbon. (2) Both C-14 and OSL ages indicate that the surface of Xitaijinair Salt Lake region has suffered erosion. (3) The sediments of XT Section are composed of silicates (quartz, muscovite, clinochlore and albite), carbonates (calcite, dolomite, and ankertie), halite and gypsum.
DOI10.1007/s12583-016-0712-6
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文献类型期刊论文
条目标识符http://ir.isl.ac.cn/handle/363002/34512
专题盐湖地质与环境实验室
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GB/T 7714
Zeng, Fangming,Xiang, Shuyuan. Geochronology and Mineral Composition of the Pleistocene Sediments in Xitaijinair Salt Lake Region, Qaidam Basin Preliminary Results[J]. JOURNAL OF EARTH SCIENCE,2017,28(4):622-627.
APA Zeng, Fangming,&Xiang, Shuyuan.(2017).Geochronology and Mineral Composition of the Pleistocene Sediments in Xitaijinair Salt Lake Region, Qaidam Basin Preliminary Results.JOURNAL OF EARTH SCIENCE,28(4),622-627.
MLA Zeng, Fangming,et al."Geochronology and Mineral Composition of the Pleistocene Sediments in Xitaijinair Salt Lake Region, Qaidam Basin Preliminary Results".JOURNAL OF EARTH SCIENCE 28.4(2017):622-627.
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