Zobrazit minimální záznam

dc.contributor.authorChmielová, Marta
dc.contributor.authorMartinec, Petr
dc.contributor.authorWeiss, Zdeněk
dc.date.accessioned2007-09-03T12:16:18Z
dc.date.available2007-09-03T12:16:18Z
dc.date.issued1997
dc.identifier.citationEuropean journal of mineralogy. 1997, vol. 9, no. 2, p. 403-409.en
dc.identifier.issn0935-1221
dc.identifier.urihttp://hdl.handle.net/10084/62447
dc.language.isoenen
dc.publisherE. Schweizerbart'sche Verlagsbuchhandlungen
dc.relation.ispartofseriesEuropean journal of mineralogyen
dc.relation.urihttp://eurjmin.geoscienceworld.org/cgi/content/abstract/9/2/403
dc.subjectAlm-Py-Gr garnetsen
dc.subjectXRD powder-patternsen
dc.subjectcomposition predictionen
dc.titleAlmandine-pyrope-grossular garnets: A method for estimating their composition using X-ray powder diffraction patternsen
dc.typearticleen
dc.identifier.locationNení ve fondu ÚKen
dc.description.abstract-enCalculated XRD powder patterns for several compositions in the Alm-Py-Gr ternary system were used to provide two identification diagrams for the composition of almandine-pyrope-grossular garnets. The first diagram is based on the changes of calculated Theta(332) (the diffraction angle of the 332 reflection) and of the intensity ratio of the 332 and 420 reflections (I-332/I-420). The second one is based on the changes of calculated Theta(444) and of the intensity ratio I-642/I-332. Six samples of natural garnets with different compositions determined by electron microprobe analysis were selected to check the reliability of the identification diagrams.en
dc.identifier.wosA1997WQ14100016


Soubory tohoto záznamu

SouboryVelikostFormátZobrazit

K tomuto záznamu nejsou připojeny žádné soubory.

Tento záznam se objevuje v následujících kolekcích

Zobrazit minimální záznam