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 | |
Zan, JB (昝金波); Fang, XM (方小敏); Yang, SL (杨胜利); Yan, MD (颜茂都); 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. | |
Source Publication | QUATERNARY INTERNATIONAL |
2013 | |
Volume | 313Issue:0Pages:210-217 |
Subject Area | 地质学 |
WOS ID | WOS:000327171200021 |
Indexed By | SCI |
Cooperation Status | 国际 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.itpcas.ac.cn/handle/131C11/2699 |
Collection | 图书馆 |
Corresponding Author | 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. |
Recommended Citation 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 ,&Zan, JB .(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. |
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