中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
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

文献类型:期刊论文

作者H. Xu ; Y.T. Hong ; Q.H. Lin ; Y.X. Zhu ; B. Hong ; H.B. Jiang
刊名Palaeogeography, Palaeoclimatology, Palaeoecology
出版日期2006
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
公开日期2011-06-13 ; 2011-07-15
源URL[http://210.72.146.199/handle/361006/2452]  
专题地球环境研究所_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,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[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.

入库方式: OAI收割

来源:地球环境研究所

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