MINERAL PHYSICS: THE ATOMIC, MESOSCOPIC AND MACROSCOPIC PERSPECTIVE

dc.contributor.author	Salje E.K.H.
dc.contributor.author	Rios S.
dc.date.accessioned	2021-06-18T05:48:30Z
dc.date.available	2021-06-18T05:48:30Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=14222410
dc.identifier.citation	Mineralogical Magazine, 2002, 66, 5, 733-744
dc.identifier.issn	0026-461X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/29114
dc.description.abstract	The macroscopic behaviour of minerals is not always directly related to their crystalline structure at the atomic scale but often depends explicitly on mesoscopic (nanometer–micrometer) features. This paper reviews various cases where the macroscopic phenomena differ from those of the bulk, with structural and chemical variations related to: domain walls, leading to enhanced or reduced transport properties; surfaces controlling growth morphologies; and radiation-damaged minerals where the interface between the amorphous and crystalline phase is believed to play a key role in hydrothermal leaching behaviour. Minerals explicitly discussed are: quartz, agate, hydroxylapatite, cordierite and metamict zircon.
dc.subject	mineral physics
dc.subject	mesoscopic features
dc.subject	domain walls
dc.subject	ionic transport
dc.subject	growth morphologies
dc.subject	radiation damage
dc.subject	silica polymorphs
dc.subject	cordierite
dc.subject	zircon
dc.title	MINERAL PHYSICS: THE ATOMIC, MESOSCOPIC AND MACROSCOPIC PERSPECTIVE
dc.type	Статья

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