中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change

文献类型:期刊论文

作者Z.D. Jin ; M.J. Bickle ; H.J. Chapman ; J.M. Yu ; S.M. Wang ; S.Y. Chen
刊名Palaeogeography, Palaeoclimatology, Palaeoecology
出版日期2009
卷号280期号:3-4页码:406-414
关键词Indian monsoon Ostracod shell Stable isotopes Lake sediment Central Tibetan Plateau
公开日期2011-05-17 ; 2011-05-18
源URL[http://210.72.146.199/handle/361006/2297]  
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
Z.D. Jin,M.J. Bickle,H.J. Chapman,et al. Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2009,280(3-4):406-414.
APA Z.D. Jin,M.J. Bickle,H.J. Chapman,J.M. Yu,S.M. Wang,&S.Y. Chen.(2009).Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change.Palaeogeography, Palaeoclimatology, Palaeoecology,280(3-4),406-414.
MLA Z.D. Jin,et al."Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change".Palaeogeography, Palaeoclimatology, Palaeoecology 280.3-4(2009):406-414.

入库方式: OAI收割

来源:地球环境研究所

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