Magnetostratigraphy of a Loess-Paleosol Sequence from Higher Terrace of the Daduhe River in the Eastern Margin of the Tibetan Plateau and Its Geological Significance

被引：0
|
作者：
QIAO Yansong [1 ,2 ]
WANG Yan [1 ]
YAO Haitao [1 ]
QI Lin [1 ,3 ]
HE Ze Xin [1 ,3 ]
CHENG Yu [1 ]
PENG Shasha [1 ,3 ]
GE Junyi [4 ]
机构：
[1] Institute of Geomechanics, Chinese Academy of Geological Sciences
[2] Key Laboratory of Neotectonic Movement & Geohazard
[3] School of Earth Sciences and Resources, China University of Geosciences
[4] Key Laboratory of Vertebrate Evolution and Human Origins of the Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences
来源：
Acta Geologica Sinica(English Edition) | 2015年 / 01期
基金：
中国国家自然科学基金;
关键词：
In; Magnetostratigraphy of a Loess-Paleosol Sequence from Higher Terrace of the Daduhe River in the Eastern Margin of the Tibetan Plateau and Its Geological Significance;
D O I：
暂无
中图分类号：
P539.3 [磁性地层学];
学科分类号：
070903 ;
摘要：
The eolian deposits distributed in the river valleys in the eastern margin of the Tibetan Plateau(TP)are very useful in neotectonic and paleoclimatic studies.Firstly,the climate in the eastern margin of the TP is mainly controlled by the Indian summer monsoon,and detailed studies on the loess-paleosol sequences in this region can provide valuable terrestrial evidence of past changes in the Indian summer monsoon.Secondly,the river terraces in the eastern margin of the TP are considered to be a sensitive recorder of neotectonism to reflect the timing and amplitude of the TP uplift.The formation ages of these
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页码：316 / 317
页数：2
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