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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/7963
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dc.contributor.authorZelek-Pogudz, S.-
dc.contributor.authorZubko, Maciej-
dc.contributor.authorPieczka, A.-
dc.date.accessioned2019-01-25T07:04:03Z-
dc.date.available2019-01-25T07:04:03Z-
dc.date.issued2016-
dc.identifier.citationActa Physica Polonica. A, Vol. 130, nr 4 (2016), s. 898-900pl_PL
dc.identifier.issn0587-4246-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/7963-
dc.description.abstractThe studied beryl crystals came from the Julianna pegmatitic system exposed in the Dolnoslaskie Surowce Skalne S.A. quarry at Piława Górna. This mineral occurs here in various forms and colours (green, yellow, white, pinkish and blue) in almost all pegmatite bodies. The paper describes the relationship between the structure and chemical composition of different coloured beryl crystals.pl_PL
dc.language.isoenpl_PL
dc.rightsUznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/pl/*
dc.subjectRietveld methodpl_PL
dc.subjectberylpl_PL
dc.titleThe Rietveld Refinement of Beryls from Pegmatitic System at Piława Górna, Góry Sowie Block, SW Polandpl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.relation.journalActa Physica Polonica. Apl_PL
dc.identifier.doi10.12693/APhysPolA.130.898-
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