Palaeomonsoon variability in the southern fringe of the Badain jaran Desert, China, since 130 ka BP
文献类型：期刊论文
| 作者 | Gao, QZ ; Tao, Z ; Li, BS ; Jin, HL ; Zou, XY ; Zhang, YC ; Dong, GR |
| 刊名 | EARTH SURFACE PROCESSES AND LANDFORMS
 |
| 出版日期 | 2006 |
| 卷号 | 31期号:3页码:265-283 |
| 关键词 | eastern Asian monsoon transitional zone between desert and loess areas fluvial and lacustrine deposits Late Pleistocene Epoch Badain Jaran Desert |
| ISSN号 | 0197-9337 |
| 通讯作者 | eesgqz@zsu.edu.cn |
| 中文摘要 | Taking the Chagelebulu Stratigraphic Profile as a typical example, a comprehensive study has been conducted to elucidate the palaeoclimatic and geomorphic evolution patterns in the southern fringe of (lie Badain Jaran Desert, which were found to be complex and polycyclic in the past 130 ka. However, the fluctuating magnitude is not as remarkable as that in the eastern China sandy region. The shift in climate from interglacial to glacial and the uplift process of the Qinghai-Xizang Plateau are the two leading forces driving the evolution of the climate and desert landforms in this area. Seventeen cycles of cold, dry and warm, humid climatic stages were recognized in the Upper Pleistocene Series of the profile. The sharp uplift of the Qinghai-Xizang Plateau superimposed a cool and arid climatic trend in this area. As a result of the climatic changes, the desert in this area has undergone multiple stages of expansion and contraction since 130 ka BP. The middle Holocene Epoch and the early stage of the Late Pleistocene Period were the main periods when the sand dunes became stabilized, and the early and late phases of the Holocene Epoch and late phase of the Pleistocene Epoch were the main periods when the previously stabilized sand dunes became mobile. The late phase of the Pleistocene Epoch was the most mobile stage, when the aeolian sand activities formed the essential geomorphic pattern (if the Badain Jaran Desert. Copyright (c) 2005 John Wiley & Sons, Ltd. |
| 学科主题 | Geography, Physical; Geosciences, Multidisciplinary |
| 收录类别 | SCI |
| 原文出处 | JOHN WILEY & SONS LTD |
| WOS记录号 | WOS:000236447000001 |
| 公开日期 | 2011-07-03 |
| 源URL | [http://ir.scsio.ac.cn/handle/344004/4446]  |
| 专题 | 南海海洋研究所_中科院边缘海地质重点实验室 |
| 推荐引用方式 GB/T 7714 | Gao, QZ,Tao, Z,Li, BS,et al. Palaeomonsoon variability in the southern fringe of the Badain jaran Desert, China, since 130 ka BP[J]. EARTH SURFACE PROCESSES AND LANDFORMS,2006,31(3):265-283. |
| APA | Gao, QZ.,Tao, Z.,Li, BS.,Jin, HL.,Zou, XY.,...&Dong, GR.(2006).Palaeomonsoon variability in the southern fringe of the Badain jaran Desert, China, since 130 ka BP.EARTH SURFACE PROCESSES AND LANDFORMS,31(3),265-283. |
| MLA | Gao, QZ,et al."Palaeomonsoon variability in the southern fringe of the Badain jaran Desert, China, since 130 ka BP".EARTH SURFACE PROCESSES AND LANDFORMS 31.3(2006):265-283. |
入库方式： OAI收割
来源：南海海洋研究所
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