Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments | |
Sun, JM; Liu, TS | |
刊名 | EARTH AND PLANETARY SCIENCE LETTERS |
2000-08-15 | |
卷号 | 180期号:3-4页码:287-296 |
关键词 | magnetic susceptibility Loess Plateau Loess genesis |
ISSN号 | 0012-821X |
文献子类 | Article |
英文摘要 | In most Chinese loess-paleosol sequences, high magnetic susceptibility values are found in the soil horizons, with low values in the loess layers. The susceptibility signal has been widely used as a proxy climatic indicator. However, both the causes and mechanisms which control susceptibility still remain controversial. Our recent studies challenge some earlier interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments. First, the prevailing hypothesis of pedogenic origin cannot totally account for the susceptibility variations in many sections. Second, in some cases, the principal carrier of the magnetization seems not to be the ultrafine pedogenic minerals, rather coarse lithogenic magnetic minerals derived from local sources can also contribute significantly to the susceptibility signal. Finally, not all the Chinese soils have higher susceptibility values than that of loess or sand layers, opposite relationships do exist. It is concluded that the source and causes of susceptibility may be different from site to site or even at different times at a given site. Any single hypothesis cannot completely account for the susceptibility variations in the Chinese Loess Plateau and its surrounding regions. Besides the previous explanations of carbonate leaching, pedogenic processes and organic decomposition, the contribution of source materials to magnetic susceptibility must also be taken into account. (C) 2000 Elsevier Science B.V. All rights reserved. |
WOS关键词 | MU US DESERT ; LOESS PLATEAU ; GRAINED MAGNETITE ; LATE QUATERNARY ; RECORD ; DEPOSITS ; STRATIGRAPHY ; PALEOSOLS ; SOILS ; PALEOCLIMATE |
WOS研究方向 | Geochemistry & Geophysics |
语种 | 英语 |
出版者 | ELSEVIER SCIENCE BV |
WOS记录号 | WOS:000088736000005 |
内容类型 | 期刊论文 |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/76145] |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Sun, JM |
作者单位 | Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Sun, JM,Liu, TS. Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments[J]. EARTH AND PLANETARY SCIENCE LETTERS,2000,180(3-4):287-296. |
APA | Sun, JM,&Liu, TS.(2000).Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments.EARTH AND PLANETARY SCIENCE LETTERS,180(3-4),287-296. |
MLA | Sun, JM,et al."Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments".EARTH AND PLANETARY SCIENCE LETTERS 180.3-4(2000):287-296. |
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