| Tibetan uplift intensified the 400 k.y. signal in paleoclimate records at 4 Ma | |
| Nie; JS (Nie; Junsheng); King; JW (King; John W.); Fang XM (方小敏) | |
| Source Publication | GEOLOGICAL SOCIETY OF AMERICA BULLETIN
 |
| 2008 | |
| Volume | 120Issue:9-10Pages:1338-1344 |
| Subject Area | 地球科学 |
| WOS ID | WOS:000258934900016 |
| Language | 英语 |
| Indexed By | SCI |
| Keyword | Chinese Loess Plateau Resolution Magneto Stratigraphy Red Clay Sequence Northern-hemisphere Thermohaline Circulation Astronomical Timescale Qinghai Province Ice Volume Myr Ago Climate |
| Cooperation Status | 其它 |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.itpcas.ac.cn/handle/131C11/642 |
| Collection | 图书馆 |
| Recommended Citation GB/T 7714 | Nie,JS (Nie,Junsheng),et al. Tibetan uplift intensified the 400 k.y. signal in paleoclimate records at 4 Ma[J]. GEOLOGICAL SOCIETY OF AMERICA BULLETIN,2008,120(9-10):1338-1344. |
| APA | Nie.,JS .,Junsheng).,King.,JW .,...&Fang XM .(2008).Tibetan uplift intensified the 400 k.y. signal in paleoclimate records at 4 Ma.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,120(9-10),1338-1344. |
| MLA | Nie,et al."Tibetan uplift intensified the 400 k.y. signal in paleoclimate records at 4 Ma".GEOLOGICAL SOCIETY OF AMERICA BULLETIN 120.9-10(2008):1338-1344. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| V.120(9-10) 1338-134（369KB） | 开放获取 | License | View Application Full Text | |||
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