FORMATION OF RINGWOODITE DURING SHOCK-WAVE LOADING OF TWO-MICA QUARTZ SCHIST: EXPERIMENTAL DATA

dc.contributor.author	Kozlov E.A.
dc.contributor.author	Sazonova L.V.
dc.contributor.author	Fel'dman V.I.
dc.contributor.author	Dubrovinskaya N.A.
dc.contributor.author	Dubrovinskii L.S.
dc.date.accessioned	2022-01-15T07:43:07Z
dc.date.available	2022-01-15T07:43:07Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13438641
dc.identifier.citation	Doklady Earth Sciences, 2003, 390, 4, 571-573
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34337
dc.description.abstract	Ringwoodite, a compact modification of olivine (γ-olivine), was experimentally synthesized under static loads (within the interval 6-24 GPa, depending on the composition and the olivine-ringwoodite conversion temperature) [1]. During the joint experimental study of shock metamorphism of rocks conducted by researchers from the All-Russia Research Institute of Technical Physics (Russian Federal Nuclear Center) and the Department of Petrology (Moscow State University), ringwoodite was first obtained under shock-wave loading conditions.
dc.title	FORMATION OF RINGWOODITE DURING SHOCK-WAVE LOADING OF TWO-MICA QUARTZ SCHIST: EXPERIMENTAL DATA
dc.type	Статья

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