Timing and provenance of loess in the Sichuan Basin, southwestern China
Timing and provenance of loess in the Sichuan Basin, southwestern China
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四川盆地黄土的形成时代和物源
DOI：
10.1016/j.palaeo.2010.03.039
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发表时间：
2010-06
期刊：
影响因子：
--
通讯作者：
Xiaomin Fang
中科院分区：
文献类型：
--
作者：
Shengli Yang;Xiaomin Fang
地貌、沉积/土壤学、粒度分布和石英氧同位素比值共同表明了成都粘土的风成成因及其在青藏高原上的主要源区。成都粘土华盖黄土剖面（位于安昌河最高阶地）的磁地层学表明，其沉积开始于825ka BP左右。这表明当时青藏高原的快速抬升与现在类似的环流系统的建立有关。
Loess-like sediments (locally called the Chengdu Clay) are widely distributed in the Sichuan Basin, at the eastern margin of the Tibetan Plateau (TP), southwest China. Geomorphology, sedimentology/pedology, grain size distributions and quartz oxygen isotopic ratios collectively demonstrate the aeolian origin of the Chengdu Clay and its main source area on the TP. Evidence also supports its transport by the Westerlies and the Tibetan winter monsoon. The magnetostratigraphy of the Huagai loess section of the Chengdu Clay (on the highest river terrace of the Anchang He River) indicates that the sediments began accumulating at about 825ka BP. This suggests the establishment of a circulation system similar to the present-day system related to the rapid uplift of the TP at that time.
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影响因子：
4
作者：
Z. Ding;Z. Yu;N. Rutter;Tung-sheng Liu
通讯作者：
Z. Ding;Z. Yu;N. Rutter;Tung-sheng Liu
DOI：
10.1111/j.1755-6724.1936.mp15002007.x
发表时间：
2009-05
期刊：
Bulletin of The Geological Society of China
影响因子：
--
作者：
J. Thorp;D. Dye
通讯作者：
J. Thorp;D. Dye
中亚和青藏高原沙尘源区的变化：与北极涛动和西风急流的联系
影响因子：
5
作者：
通讯作者：
--
DOI：
10.1186/bf03352094
发表时间：
1998-02
期刊：
Earth, Planets and Space
影响因子：
--
作者：
Humaira Akram;Mitsuo Yoshida;M. Ahmad
通讯作者：
Humaira Akram;Mitsuo Yoshida;M. Ahmad
影响因子：
--
作者：
Xiaoyong Wang;Huayu Lu;Zhen Li;C. Deng;H. Tan;Yougui Song
通讯作者：
Xiaoyong Wang;Huayu Lu;Zhen Li;C. Deng;H. Tan;Yougui Song