Intracrystalline and grain-boundary olivine-ringwoodite (-wadsleyite) phase transitions in shocked L6 chondrites: Evidence for diffusion controlled phase transition mechanisms involving Fe and Mn

GIG OpenIR > 中科院广州地化所(-2008)

	Intracrystalline and grain-boundary olivine-ringwoodite (-wadsleyite) phase transitions in shocked L6 chondrites: Evidence for diffusion controlled phase transition mechanisms involving Fe and Mn
	El Goresy A; Ferroir T; Gillet P; Chen M; Dubrovinsky L; Simionovici A
Source Publication	69th Annual Meeting of the Meteoritical Society
	2006-08-06
Conference Date	2006-8-6
Conference Place	Zurich, SWITZERLAND
Indexed By	SCI
Language	英语
Citation statistics	Cited Times:1[WOS] [WOS Record] [Related Records in WOS]
Document Type	会议论文
Identifier	http://ir.gig.ac.cn/handle/344008/9324
Collection	中科院广州地化所(-2008)
Recommended Citation GB/T 7714	El Goresy A,Ferroir T,Gillet P,et al. Intracrystalline and grain-boundary olivine-ringwoodite (-wadsleyite) phase transitions in shocked L6 chondrites: Evidence for diffusion controlled phase transition mechanisms involving Fe and Mn[C],2006.

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