The Mossbauer spectra of prasiolite and amethyst crystals from Poland

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DC pole	Wartość	Język
dc.contributor.author	Czaja, Maria	-
dc.contributor.author	Kądziołka-Gaweł, Mariola	-
dc.contributor.author	Konefał, Adam	-
dc.contributor.author	Sitko, Rafał	-
dc.contributor.author	Teper, Ewa	-
dc.contributor.author	Mazurak, Zbigniew	-
dc.contributor.author	Sachanbiński, Michał	-
dc.date.accessioned	2018-05-22T09:18:26Z	-
dc.date.available	2018-05-22T09:18:26Z	-
dc.date.issued	2017	-
dc.identifier.citation	Physics and Chemistry of Minerals, Vol. 5 (2017), s. 365-375	pl_PL
dc.identifier.issn	0342-1791	-
dc.identifier.uri	http://hdl.handle.net/20.500.12128/3822	-
dc.description.abstract	Mössbauer spectroscopy of green (prasiolite) and violet (amethyst) quartz crystals from the Sudety Mountains (Poland) has shown that neither Fe2+ nor Fe4+ ions are present in them. Only Fe3+ ions have been identified and only in interstitial positions in channels parallel or perpendicular to the c-axis. The valence of Fe3+ ions did not change as a result of irradiation or annealing. Instead, we believe that the Fe3+ ions move within channels or between them.	pl_PL
dc.language.iso	en	pl_PL
dc.rights	Uznanie autorstwa 3.0 Polska	*
dc.rights.uri	http://creativecommons.org/licenses/by/3.0/pl/	*
dc.subject	Amethyst	pl_PL
dc.subject	Fe3+ ion	pl_PL
dc.subject	Mössbauer spectroscopy	pl_PL
dc.subject	Prasiolite	pl_PL
dc.title	The Mossbauer spectra of prasiolite and amethyst crystals from Poland	pl_PL
dc.type	info:eu-repo/semantics/article	pl_PL
dc.identifier.doi	10.1007/s00269-016-0864-z	-
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