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
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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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