IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2005-2009)
Temperature responses to quasi-100-yr solar variability during the past 6000 years based on δ18O of peat cellulose in Hongyuan,eastern Qinghai–Tibet plateau, China
H. Xu; Y.T. Hong; Q.H. Lin; Y.X. Zhu; B. Hong; H.B. Jiang
2006
Source PublicationPalaeogeography, Palaeoclimatology, Palaeoecology
Volume230Issue:1-2Pages:155-164
KeywordPeat Oxygen Isotopic Composition Temperature Solar Activity Qinghai–tibet Plateau China
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/2452
Collection黄土与第四纪地质国家重点实验室(2005-2009)
Recommended Citation
GB/T 7714
H. Xu,Y.T. Hong,Q.H. Lin,等. Temperature responses to quasi-100-yr solar variability during the past 6000 years based on δ18O of peat cellulose in Hongyuan,eastern Qinghai–Tibet plateau, China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2006,230(1-2):155-164.
APA H. Xu,Y.T. Hong,Q.H. Lin,Y.X. Zhu,B. Hong,&H.B. Jiang.(2006).Temperature responses to quasi-100-yr solar variability during the past 6000 years based on δ18O of peat cellulose in Hongyuan,eastern Qinghai–Tibet plateau, China.Palaeogeography, Palaeoclimatology, Palaeoecology,230(1-2),155-164.
MLA H. Xu,et al."Temperature responses to quasi-100-yr solar variability during the past 6000 years based on δ18O of peat cellulose in Hongyuan,eastern Qinghai–Tibet plateau, China".Palaeogeography, Palaeoclimatology, Palaeoecology 230.1-2(2006):155-164.
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