GIG OpenIR  > 中科院广州地化所(-2008)
Xu JF; Wang Q; Yu XY
Geochemistry of high-Mg andesites and adakitic andesite from the Sanchazi block of the Mian-Lue ophiolitic melange in the Qinling Mountains, central China: Evidence of partial melting of the subducted Paleo-Tethyan crust
Source PublicationGeochemical Journal
ISSN0016-7002
2000
Volume34Issue:5Pages:359-377
Indexed Bysci
Language英语
WOS IDWOS:000090080400004
Citation statistics
Cited Times:60[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/11585
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714
Xu JF,Wang Q,Yu XY. Geochemistry of high-Mg andesites and adakitic andesite from the Sanchazi block of the Mian-Lue ophiolitic melange in the Qinling Mountains, central China: Evidence of partial melting of the subducted Paleo-Tethyan crust[J]. Geochemical Journal,2000,34(5):359-377.
APA Xu JF,Wang Q,&Yu XY.(2000).Geochemistry of high-Mg andesites and adakitic andesite from the Sanchazi block of the Mian-Lue ophiolitic melange in the Qinling Mountains, central China: Evidence of partial melting of the subducted Paleo-Tethyan crust.Geochemical Journal,34(5),359-377.
MLA Xu JF,et al."Geochemistry of high-Mg andesites and adakitic andesite from the Sanchazi block of the Mian-Lue ophiolitic melange in the Qinling Mountains, central China: Evidence of partial melting of the subducted Paleo-Tethyan crust".Geochemical Journal 34.5(2000):359-377.
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