IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2005-2009)
Evaluation of oxygen isotopes in carbonate as an indicator of lake evolution in arid areas: The modern Qinghai Lake, Qinghai–Tibet Plateau
W.G. Liu; X.Z. Li; L. Zhang; Z.S. An; L.M. Xu
2009
Source PublicationCHEMICAL GEOLOGY
Volume268Issue:1-2Pages:126-136
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/2314
Collection黄土与第四纪地质国家重点实验室(2005-2009)
Recommended Citation
GB/T 7714
W.G. Liu,X.Z. Li,L. Zhang,等. Evaluation of oxygen isotopes in carbonate as an indicator of lake evolution in arid areas: The modern Qinghai Lake, Qinghai–Tibet Plateau[J]. CHEMICAL GEOLOGY,2009,268(1-2):126-136.
APA W.G. Liu,X.Z. Li,L. Zhang,Z.S. An,&L.M. Xu.(2009).Evaluation of oxygen isotopes in carbonate as an indicator of lake evolution in arid areas: The modern Qinghai Lake, Qinghai–Tibet Plateau.CHEMICAL GEOLOGY,268(1-2),126-136.
MLA W.G. Liu,et al."Evaluation of oxygen isotopes in carbonate as an indicator of lake evolution in arid areas: The modern Qinghai Lake, Qinghai–Tibet Plateau".CHEMICAL GEOLOGY 268.1-2(2009):126-136.
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