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DOI | 10.1130/G32296.1 |
Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications | |
Pullen, Alex; Kapp, Paul; McCallister, Andrew T.; Chang, Hong; Gehrels, George E.; Garzione, Carmala N.; Heermance, Richard V.; Ding, Lin | |
通讯作者 | Pullen, A (通讯作者) |
发表日期 | 2011 |
ISSN | 0091-7613 |
起始页码 | 1031 |
结束页码 | 1034 |
卷号 | 39期号:11 |
英文摘要 | The Chinese Loess Plateau of central Asia is composed of interbedded loess and paleosol layers, deposited during glacial and interglacial cycles, respectively, during the past similar to 2.5 m.y. Understanding the provenance of loess is fundamental to reconstructing wind patterns during Quaternary glacial periods. We determined and compared U-Pb ages on zircon crystals from Loess Plateau strata and potential source areas. The results indicate that the loess was largely derived from the Qaidam Basin and the northern Tibetan Plateau to the west, both of which exhibit spatially extensive geomorphic landforms indicative of past (interpreted as pre-Holocene) wind erosion and/or deflation by westerly winds. This challenges the current paradigm that the loess of the Chinese Loess Plateau was largely sourced from deserts located to the northwest, as observed in the modern interglacial climate. We propose that during glacial periods, the mean annual positions of the polar jet streams were shifted equatorward, resulting in more southerly tracks for dust-generating storms and suppression of the East Asian monsoon by inhibiting the subtropical jet from shifting northward across the Tibetan Plateau. |
关键词 | GARZE FOLD BELTTECTONIC EVOLUTIONISOTOPE GEOCHEMISTRYWESTERLY JETASIAN DUSTDEEP-SEAPROVENANCECLIMATERECORDCONSTRAINTS |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geology |
WOS记录号 | WOS:000296607600012 |
来源期刊 | GEOLOGY |
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/257947 |
推荐引用方式 GB/T 7714 | Pullen, Alex,Kapp, Paul,McCallister, Andrew T.,et al. Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications[J]. 中国科学院青藏高原研究所,2011,39(11). |
APA | Pullen, Alex.,Kapp, Paul.,McCallister, Andrew T..,Chang, Hong.,Gehrels, George E..,...&Ding, Lin.(2011).Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications.GEOLOGY,39(11). |
MLA | Pullen, Alex,et al."Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications".GEOLOGY 39.11(2011). |
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