首页|期刊导航|中国地球化学学报（英文版）|Magnetic susceptibility of the Xifeng section and its paleoclimate significance
中国地球化学学报（英文版）2009，Vol.28Issue(1)：81-85,5.DOI:10.1007/s11631-009-0081-2
Magnetic susceptibility of the Xifeng section and its paleoclimate significance
Magnetic susceptibility of the Xifeng section and its paleoclimate significance
摘要
Abstract
Magnetic susceptibility (MS) is one of the most important indicators of the East-Asia summer monsoon. Presented in this study is a high resolution magnetic susceptibility record from the Xifeng section, which consists of Quaternary loess-paleosol sequence and Pliocene red clay. Variations in magnetic susceptibility are well correlated with the δ18O record in deep-sea sediments and the eolian flux of Greenland. The climatic evolution in the Xifeng section shows that since the Late Tertiary, the driving force of the East-Asia paleo-monsoon is correlated with solar radiation on a 10-ka time scale.关键词
magnetic susceptibility/paleoclimate/Xifeng/loess-paleosol/red clayKey words
magnetic susceptibility/paleoclimate/Xifeng/loess-paleosol/red clay分类
天文与地球科学引用本文复制引用
SUN Yubing,CHEN Tianhu,XIE Qiaoqin..Magnetic susceptibility of the Xifeng section and its paleoclimate significance[J].中国地球化学学报（英文版）,2009,28(1):81-85,5.基金项目
This study was supported by the National Natural Science Foundation of China (Grant Nos. 40331001 and 40472026). （Grant Nos. 40331001 and 40472026）
