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Schreyer, W., Bernhardt, H.-J., Medenbach, O. (1992) Petrologic evidence for a rhodochrosite precursor of spessartine in coticules of the Venn-Stavelot Massif, Belgium. Mineralogical Magazine, 56 (385) 527-532 doi:10.1180/minmag.1992.056.385.08

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Reference TypeJournal (article/letter/editorial)
TitlePetrologic evidence for a rhodochrosite precursor of spessartine in coticules of the Venn-Stavelot Massif, Belgium
JournalMineralogical MagazineISSN0026-461X
AuthorsSchreyer, W.Author
Bernhardt, H.-J.Author
Medenbach, O.Author
Year1992 (December)Volume56
Page(s)527-532Issue385
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-385-527.pdf+
DOIdoi:10.1180/minmag.1992.056.385.08Search in ResearchGate
Mindat Ref. ID1866Long-form Identifiermindat:1:5:1866:5
GUID89f5acd3-a080-4f73-bc92-449fd1ae0006
Full ReferenceSchreyer, W., Bernhardt, H.-J., Medenbach, O. (1992) Petrologic evidence for a rhodochrosite precursor of spessartine in coticules of the Venn-Stavelot Massif, Belgium. Mineralogical Magazine, 56 (385) 527-532 doi:10.1180/minmag.1992.056.385.08
Plain TextSchreyer, W., Bernhardt, H.-J., Medenbach, O. (1992) Petrologic evidence for a rhodochrosite precursor of spessartine in coticules of the Venn-Stavelot Massif, Belgium. Mineralogical Magazine, 56 (385) 527-532 doi:10.1180/minmag.1992.056.385.08
In(1992, December) Mineralogical Magazine Vol. 56 (385) Mineralogical Society
Abstract/NotesAbstractMinute CaMg-bearing rhodochrosite inclusions were discovered in spessartine crystals of small coticule globules enclosed within redschists that form the country rock of the famous coticule bands of Belgium. This points to a former metamorphic reaction relationship between the two minerals, such as rhodochrosite + pyrophyllite = spessartine + quartz + CO2 + H2O. The coexistence of spessartine with Mg-chlorite in the coticule globule could also indicate more complex reactions such as rhodochrosite + sudoite + quartz = spessartine + Mg-chlorite + CO2 + H2O. Our finding casts some doubt on the suggestion by Kramm (1976) that spessartine formed from Mn-montmorillonite in previously glassy volcanic tufts.


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