SHORT-RANGE MOBILIZATION OF ELEMENTS IN THE BIOTITE ZONE OF CONTACT AUREOLE OF THE KHARLOVO GABBRO MASSIF (RUSSIA)

dc.contributor.author	Likhanov I.I.
dc.contributor.author	Reverdatto V.V.
dc.contributor.author	Memmi I.
dc.date.accessioned	2020-11-19T06:43:30Z
dc.date.available	2020-11-19T06:43:30Z
dc.date.issued	1994
dc.description.abstract	Mass balance and compositional variation in the outer part of the contact aureole shows that mass transfer of the main petrogenetic components was confined to small domains of a few hundredths of mm3 in chlorite-biotite-mica and epidote-plagioclase-titanomagnetite aggregates. The chemical homogeneity of the environment was practically unaffected by the thermal metamorphism.
dc.identifier	https://elibrary.ru/item.asp?id=26355330
dc.identifier.citation	European Journal of Mineralogy, 1994, , 1, 133-144
dc.identifier.issn	0935-1221
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/19025
dc.title	SHORT-RANGE MOBILIZATION OF ELEMENTS IN THE BIOTITE ZONE OF CONTACT AUREOLE OF THE KHARLOVO GABBRO MASSIF (RUSSIA)
dc.type	Статья

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