Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau
文献类型：期刊论文
| 作者 | Zan, JB (昝金波) ; Fang, XM (方小敏) ; Yang, SL (杨胜利) ; Yan, MD (颜茂都) |
| 刊名 | QUATERNARY INTERNATIONAL
 |
| 出版日期 | 2013 |
| 卷号 | 313期号:0页码:210-217 |
| 通讯作者 | Zan, JB (通讯作者),Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Shuangqing Rd 18, Beijing 100085, Peoples R China. |
| 合作状况 | 国际 |
| 学科主题 | 地质学 |
| 收录类别 | SCI |
| WOS记录号 | WOS:000327171200021 |
| 公开日期 | 2014-05-28 |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/2699]  |
| 专题 | 青藏高原研究所_图书馆 |
| 推荐引用方式 GB/T 7714 | Zan, JB ,Fang, XM ,Yang, SL ,et al. Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau[J]. QUATERNARY INTERNATIONAL,2013,313(0):210-217. |
| APA | Zan, JB ,Fang, XM ,Yang, SL ,&Yan, MD .(2013).Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau.QUATERNARY INTERNATIONAL,313(0),210-217. |
| MLA | Zan, JB ,et al."Evolution of the arid climate in High Asia since similar to 1 Ma: Evidence from loess deposits on the surface and rims of the Tibetan Plateau".QUATERNARY INTERNATIONAL 313.0(2013):210-217. |
入库方式： OAI收割
来源：青藏高原研究所
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