An Eocene-Miocene continuous rock magnetic record from the sediments in the Xining Basin, NW China: indication for Cenozoic persistent drying driven by global cooling and Tibetan Plateau uplift
文献类型：期刊论文
| 作者 | Fang, XM (Fang, Xiaomin)1,2; Zan, JB (Zan, Jinbo)1,2; Appel, E (Appel, Erwin)3; Lu, Y (Lu, Yin)1,2; Song, CH (Song, Chunhui)4,5; Dai, S (Dai, Shuang)4,5; Tuo, SB (Tuo, Shibo)4,5 |
| 刊名 | GEOPHYSICAL JOURNAL INTERNATIONAL
 |
| 出版日期 | 2015 |
| 卷号 | 201期号:1页码:78-89 |
| 通讯作者 | Fang, XM |
| 合作状况 | 国际 |
| 学科主题 | 地质学 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000355153000006 |
| 源URL | [http://ir.itpcas.ac.cn/handle/131C11/7342]  |
| 专题 | 青藏高原研究所_图书馆 |
| 作者单位 | 1.Chinese Acad Sci, Inst Tibetan Plateau Res, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China 3.Univ Tubingen, Dept Geosci, D-72074 Tubingen, Germany 4.Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China 5.Lanzhou Univ, Key Lab Western Chinas Environm Syst MOE, Lanzhou 730000, Peoples R China |
| 推荐引用方式 GB/T 7714 | Fang, XM ,Zan, JB ,Appel, E ,et al. An Eocene-Miocene continuous rock magnetic record from the sediments in the Xining Basin, NW China: indication for Cenozoic persistent drying driven by global cooling and Tibetan Plateau uplift[J]. GEOPHYSICAL JOURNAL INTERNATIONAL,2015,201(1):78-89. |
| APA | Fang, XM .,Zan, JB .,Appel, E .,Lu, Y .,Song, CH .,...&Tuo, SB .(2015).An Eocene-Miocene continuous rock magnetic record from the sediments in the Xining Basin, NW China: indication for Cenozoic persistent drying driven by global cooling and Tibetan Plateau uplift.GEOPHYSICAL JOURNAL INTERNATIONAL,201(1),78-89. |
| MLA | Fang, XM ,et al."An Eocene-Miocene continuous rock magnetic record from the sediments in the Xining Basin, NW China: indication for Cenozoic persistent drying driven by global cooling and Tibetan Plateau uplift".GEOPHYSICAL JOURNAL INTERNATIONAL 201.1(2015):78-89. |
入库方式： OAI收割
来源：青藏高原研究所
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