Structural evolution of the Neogene Gar Evaporite minerals and geochemistry of the upper 400 m sediments in a core from the Western Qaidam Basin, Tibet
文献类型：期刊论文
| 作者 | Fang XM(方小敏) ; Gao SP(高少鹏)
|
| 刊名 | QUATERNARY INTERNATIONAL
 |
| 出版日期 | 2010 |
| 卷号 | 218期号:1-2页码:176-189 |
| 关键词 | NORTHERN TIBET QUATERNARY LACUSTRINE NORTHWESTERN CHINA TECTONIC UPLIFT CLIMATIC-CHANGE SALT-LAKE NW CHINA DEPOSITS GYPSUM EVOLUTION |
| 通讯作者 | 方小敏 |
| 合作状况 | 国际 |
| 学科主题 | 地球科学 |
| 收录类别 | SCI |
| 语种 | 英语 |
| 公开日期 | 2011-05-05 |
| 源URL | [http://ir.itpcas.ac.cn:8080/handle/131C11/1489]  |
| 专题 | 青藏高原研究所_图书馆 |
| 推荐引用方式 GB/T 7714 | Fang XM,Gao SP. Structural evolution of the Neogene Gar Evaporite minerals and geochemistry of the upper 400 m sediments in a core from the Western Qaidam Basin, Tibet[J]. QUATERNARY INTERNATIONAL,2010,218(1-2):176-189. |
| APA | Fang XM,&Gao SP.(2010).Structural evolution of the Neogene Gar Evaporite minerals and geochemistry of the upper 400 m sediments in a core from the Western Qaidam Basin, Tibet.QUATERNARY INTERNATIONAL,218(1-2),176-189. |
| MLA | Fang XM,et al."Structural evolution of the Neogene Gar Evaporite minerals and geochemistry of the upper 400 m sediments in a core from the Western Qaidam Basin, Tibet".QUATERNARY INTERNATIONAL 218.1-2(2010):176-189. |
入库方式： OAI收割
来源：青藏高原研究所
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