Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, southern Siberia
文献类型：期刊论文
| 作者 | Zhu, RX; Matasova, G; Kazansky, A; Zykina, V; Sun, JM |
| 刊名 | GEOPHYSICAL JOURNAL INTERNATIONAL
 |
| 出版日期 | 2003 |
| 卷号 | 152期号:2页码:335-343 |
| ISSN号 | 0956-540X |
| 关键词 | Buried Soil Loess Palaeoclimate Rock Magnetism Siberia |
| 文献子类 | Article |
| 英文摘要 | Detailed rock magnetic investigations, grain size determination and X-ray diffraction were carried out on loess and buried soils of the last glacial-interglacial cycle from Kurtak, southern Siberia. The susceptibility and the sand fraction of >63 mum fluctuate in parallel, suggesting that the higher susceptibility values in the loess horizons are mainly associated with the coarse size fraction. The frequency dependence of the magnetic susceptibility of the loess and buried soils is very low and uniform, indicating the absence of superparamagnetic grains and negligible pedogenically induced enhancement of magnetic susceptibility. The magnetic assemblage is dominated by multidomain-like magnetite grains. Maghemite and haematite are also present in the buried soils and loess horizons. Goethite may have been formed from gleying or water-logging processes under a cooler and more humid climate. The coarse magnetite grains, which contribute significantly to magnetic susceptibility, are probably carried by valley winds and derived from local sources. Thus, the coarser magnetite grains with higher susceptibility values in the loess horizons could mainly reflect stronger wind intensity during cold and semi-arid conditions, and the consequent ease with which dense magnetite particles can be transported. The lower susceptibility values in the buried soil horizons are mainly caused by weaker wind intensity during interglacial and interstadial periods, although post-depositional processes associated with gleying modifications are also partially responsible for the observations. |
| WOS关键词 | TEMPERATURE-DEPENDENT SUSCEPTIBILITY ; NW-SE TRANSECT ; CHINESE LOESS ; PALEOSOL SEQUENCES ; LATE QUATERNARY ; LATE PLEISTOCENE ; ALASKAN LOESS ; PLATEAU ; SEDIMENTS ; PEDOGENESIS |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| 出版者 | BLACKWELL PUBLISHING LTD |
| WOS记录号 | WOS:000180424000007 |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/78667]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Zhu, RX |
| 作者单位 | 1.Chinese Acad Sci, Palaeomagnetism Lab, Inst Geol & Geophys, Beijing 100101, Peoples R China 2.Russian Acad Sci, Inst Geol, UIGGM Siberian Div, Novosibirsk, Russia |
| 推荐引用方式 GB/T 7714 | Zhu, RX,Matasova, G,Kazansky, A,et al. Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, southern Siberia[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2003,152(2):335-343. |
| APA | Zhu, RX,Matasova, G,Kazansky, A,Zykina, V,&Sun, JM.(2003).Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, southern Siberia.GEOPHYSICAL JOURNAL INTERNATIONAL,152(2),335-343. |
| MLA | Zhu, RX,et al."Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, southern Siberia".GEOPHYSICAL JOURNAL INTERNATIONAL 152.2(2003):335-343. |
入库方式： OAI收割
来源：地质与地球物理研究所
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