Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室(2005-2009)

	Early to mid-Pleistocene ostracod δ18O and δ13C in the central Tibetan Plateau:Implication for Indian monsoon change
	Z.D. Jin; M.J. Bickle; H.J. Chapman; J.M. Yu; S.M. Wang; S.Y. Chen
	2009
发表期刊	Palaeogeography, Palaeoclimatology, Palaeoecology
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
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/2297
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	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.