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Mevel, C., Kienast, J. R. (1980) Chromian jadeite, phengite, pumpellyite, and lawsonite in a high–pressure metamorphosed gabbro from the French Alps. Mineralogical Magazine, 43 (332) 979-984 doi:10.1180/minmag.1980.043.332.04

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Reference TypeJournal (article/letter/editorial)
TitleChromian jadeite, phengite, pumpellyite, and lawsonite in a high–pressure metamorphosed gabbro from the French Alps
JournalMineralogical MagazineISSN0026-461X
AuthorsMevel, C.Author
Kienast, J. R.Author
Year1980 (December)Volume43
Issue332
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_43/43-332-979.pdf+
DOIdoi:10.1180/minmag.1980.043.332.04Search in ResearchGate
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Mindat Ref. ID3185Long-form Identifiermindat:1:5:3185:5
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Full ReferenceMevel, C., Kienast, J. R. (1980) Chromian jadeite, phengite, pumpellyite, and lawsonite in a high–pressure metamorphosed gabbro from the French Alps. Mineralogical Magazine, 43 (332) 979-984 doi:10.1180/minmag.1980.043.332.04
Plain TextMevel, C., Kienast, J. R. (1980) Chromian jadeite, phengite, pumpellyite, and lawsonite in a high–pressure metamorphosed gabbro from the French Alps. Mineralogical Magazine, 43 (332) 979-984 doi:10.1180/minmag.1980.043.332.04
In(1980, December) Mineralogical Magazine Vol. 43 (332) Mineralogical Society
Abstract/NotesSummarySmall ophiolitic bodies are enclosed in the calcschists of the Piemont zone (western Alps). They have been metamorphosed in the blueschist facies during the alpine orogeny. One of them, the Roche Noire massif, includes gabbro breccias. The magmatic mineralogy of the gabbro was plagioclase + clinopyroxene + minor chromite. There was no chemical homogenization during metamorphism because of the lack of penetrative deformation and on the site of previous chromites, chromium-rich high-pressure and low-temperature minerals (jadeite, phengite, pumpellyite, and lawsonite) were formed. The Al ⇌ Cr substitution does not affect other P- and T-dependent substitutions.


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