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Climatic variation in the Linxia basin, NE Tibetan Plateau, from 13.1 to 4.3 Ma: The stable isotope record
Fan; MJ (Fan; Majie); Dettman; DL (Dettman; David L.); Song; CH (Song; Chunhui); Fang XM(方小敏); Garzione; CN (Garzione; Carmala N.)
Source PublicationPALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
2007
Volume247Issue:3-4Pages:313-328
Subject Area自然地理学
WOS IDWOS:000246167300008
Language英语
Indexed BySCI
KeywordCHINESE LOESS PLATEAU ORGANIC-MATTER ASIAN MONSOON C/N RATIOS SOURCE INDICATORS CARBON-ISOTOPE EVOLUTION NITROGEN DIAGENESIS DOLOMITE
Cooperation Status其它
Citation statistics
Cited Times:68[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/1013
Collection图书馆
Recommended Citation
GB/T 7714
Fan,MJ (Fan,Majie),et al. Climatic variation in the Linxia basin, NE Tibetan Plateau, from 13.1 to 4.3 Ma: The stable isotope record[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2007,247(3-4):313-328.
APA Fan.,MJ .,Majie).,Dettman.,DL .,...&Carmala N.).(2007).Climatic variation in the Linxia basin, NE Tibetan Plateau, from 13.1 to 4.3 Ma: The stable isotope record.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,247(3-4),313-328.
MLA Fan,et al."Climatic variation in the Linxia basin, NE Tibetan Plateau, from 13.1 to 4.3 Ma: The stable isotope record".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 247.3-4(2007):313-328.
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