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

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
发表期刊	Palaeogeography, Palaeoclimatology, Palaeoecology
卷号	230 期号:1-2 页码:155-164
关键词	Peat Oxygen Isotopic Composition Temperature Solar Activity Qinghai–tibet Plateau China
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/2452
专题	黄土与第四纪地质国家重点实验室(2005-2009)
推荐引用方式 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.