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 | |
Li MH(李明慧); Fang XM(方小敏); Yi CL(易朝路); Gao SP(高少鹏); Zhang WL(张伟林); Galy; A (Galy; Albert); Fang XM(方小敏) | |
Source Publication | QUATERNARY INTERNATIONAL |
2010 | |
Volume | 218Issue:1-2Pages:176-189 |
Subject Area | 地球科学 |
Language | 英语 |
Indexed By | SCI |
Keyword | Northern Tibet Quaternary Lacustrine Northwestern China Tectonic Uplift Climatic-change Salt-lake Nw China Deposits Gypsum Evolution |
Cooperation Status | 国际 |
Document Type | 期刊论文 |
Identifier | http://ir.itpcas.ac.cn/handle/131C11/1489 |
Collection | 图书馆 |
Corresponding Author | Fang XM(方小敏) |
Recommended Citation GB/T 7714 | Li MH,Fang XM,Yi CL,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[J]. QUATERNARY INTERNATIONAL,2010,218(1-2):176-189. |
APA | Li MH.,Fang XM.,Yi CL.,Gao SP.,Zhang WL.,...&方小敏.(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 | Li MH,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. |
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