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Heflik, W., Żabiński, W. (1969) A chromian hydrogrossular from Jordanów, Lower Silesia, Poland. Mineralogical Magazine, 37 (286) 241-243 doi:10.1180/minmag.1969.037.286.12

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Reference TypeJournal (article/letter/editorial)
TitleA chromian hydrogrossular from Jordanów, Lower Silesia, Poland
JournalMineralogical Magazine
AuthorsHeflik, W.Author
Żabiński, W.Author
Year1969 (June)Volume37
Issue286
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_37/37-286-241.pdf+
DOIdoi:10.1180/minmag.1969.037.286.12Search in ResearchGate
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Mindat Ref. ID6261Long-form Identifiermindat:1:5:6261:3
GUID0
Full ReferenceHeflik, W., Żabiński, W. (1969) A chromian hydrogrossular from Jordanów, Lower Silesia, Poland. Mineralogical Magazine, 37 (286) 241-243 doi:10.1180/minmag.1969.037.286.12
Plain TextHeflik, W., Żabiński, W. (1969) A chromian hydrogrossular from Jordanów, Lower Silesia, Poland. Mineralogical Magazine, 37 (286) 241-243 doi:10.1180/minmag.1969.037.286.12
In(1969, June) Mineralogical Magazine Vol. 37 (286) Mineralogical Society
Abstract/NotesSummaryA new variety of garnet, a chromian hydrogrossular, has been found in a loose block of diopside-albite rock in a quarry of serpentinite in Jordanów, Lower Silesia. Its chemical formula is given. Although the water content of this garnet barely exceeds 1 %, the X-ray, thermal, infra-red spectrophotometric, and optical examinations give evidence that this water, in the form of (OH)4 groupings, substitutes for the SiO4 tetrahedra. The chromian hydrogrossular from Jordanów belongs to the numerous calcium-rich silicates that were formed there during the process of alteration of serpentinites by lime-rich hydrothermal solutions.


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