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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 PublicationQUATERNARY INTERNATIONAL
2010
Volume218Issue:1-2Pages:176-189
Subject Area地球科学
Language英语
Indexed BySCI
KeywordNorthern 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
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/1489
Collection图书馆
Corresponding AuthorFang 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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