Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle

GIG OpenIR > 中科院广州地化所(-2008)

	Chen M; El Goresy A; Frost D; Gillet P
	Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle
Source Publication	European Journal of Mineralogy
ISSN	0935-1221
	2004
Volume	16 Issue:2 Pages:203-211
Language	英语
WOS ID	WOS:000220576500001
Indexed By	sci
Citation statistics	Cited Times:8[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/12243
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	Chen M,El Goresy A,Frost D,et al. Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle[J]. European Journal of Mineralogy,2004,16(2):203-211.
APA	Chen M,El Goresy A,Frost D,&Gillet P.(2004).Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle.European Journal of Mineralogy,16(2),203-211.
MLA	Chen M,et al."Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle".European Journal of Mineralogy 16.2(2004):203-211.

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