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 delta O-18 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
DepartmentIEECAS LLQG
Indexed Bysci
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/408
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 delta O-18 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 delta O-18 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 delta O-18 of peat cellulose in Hongyuan;eastern Qinghai-Tibet plateau;China".Palaeogeography Palaeoclimatology Palaeoecology 230.1-2(2006):155-164.
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