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DOI | 10.1016/j.jseaes.2006.10.004 |
Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau | |
Song, Yougui; Fang, Xiaomin; Torii, Masayuki; Ishikawa, Naoto; Li, Jijun; An, Zhisheng | |
发表日期 | 2007 |
ISSN | 1367-9120 |
EISSN | 1878-5786 |
起始页码 | 324 |
结束页码 | 332 |
卷号 | 30期号:2 |
英文摘要 | The Late Cenozoic red clay-loess sequence in the Chinese Loess Plateau provides a high-resolution record of palcoclimatic and tectonic changes related to the phased uplift of the Tibetan Plateau. Detailed magnetostratigraphy of a recently recovered 125-m-thick sediment sequence from the central Chinese Loess Plateau shows that the red clay began to accumulate at ca. 8.1 Ma, implying a marked drying in the interior of Asian as well as the initial establishment of the East Asian paleomonsoon regime. Prior to 3.8 Ma, the ferromagnetic mineral concentrations, as revealed by both magnetic susceptibility and S-ratios, exhibit a cyclic pattern superimposed upon a linear trend. This pattern collapsed immediately after 3.8 Ma, suggesting a change in source area. This in turn may have resulted from the reorganization of atmospheric circulation and the onset of the modern Asian monsoon, probably associated with the accelerated uplift of the Tibetan Plateau to a certain threshold elevation. (C) 2007 Elsevier Ltd. All rights reserved. |
关键词 | LATE CENOZOIC DEFORMATIONRED-EARTH FORMATIONEAST-ASIAN MONSOONLOESS PLATEAUNORTHERN-HEMISPHERELATE MIOCENEAUTONOMOUS REGIONLIUPAN SHANMYR AGOMAGNETOSTRATIGRAPHY |
英文关键词 | red clay formation; magneto stratigraphy; rock magnetism; Neogene; atmospheric circulation reorganization; Chinese Loess Plateau |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000246252000008 |
来源期刊 | JOURNAL OF ASIAN EARTH SCIENCES
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/257518 |
推荐引用方式 GB/T 7714 | Song, Yougui,Fang, Xiaomin,Torii, Masayuki,et al. Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau[J]. 中国科学院青藏高原研究所,2007,30(2). |
APA | Song, Yougui,Fang, Xiaomin,Torii, Masayuki,Ishikawa, Naoto,Li, Jijun,&An, Zhisheng.(2007).Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau.JOURNAL OF ASIAN EARTH SCIENCES,30(2). |
MLA | Song, Yougui,et al."Late Neogene rock magnetic record of climatic variation from Chinese eolian sediments related to uplift of the Tibetan Plateau".JOURNAL OF ASIAN EARTH SCIENCES 30.2(2007). |
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