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  Alkali-F-rich albite zones in evolved NYF pegmatites: the product of melt-melt immiscibility

Müller, A., Spratt, J., Thomas, R., Williamson, B. J., Seltmann, R. (2018): Alkali-F-rich albite zones in evolved NYF pegmatites: the product of melt-melt immiscibility. - Canadian Mineralogist, 56, 657-687.
https://doi.org/10.3749/canmin.1700087

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 Creators:
Müller, Axel1, Author
Spratt, John1, Author
Thomas, R.2, Author              
Williamson, Ben J.1, Author
Seltmann, Reimar1, Author
Affiliations:
1External Organizations, ou_persistent22              
24.3 Chemistry and Physics of Earth Materials, 4.0 Geomaterials, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146036              

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Free keywords: Pegmatite, albite zone, trace elements, melt inclusion, Sveconorwegian orogeny, Evje, Iveland
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 Dates: 2018
 Publication Status: Finally published
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 Identifiers: DOI: 10.3749/canmin.1700087
GFZPOF: p3 PT2 Plate Boundary Systems
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Title: Canadian Mineralogist
Source Genre: Journal, SCI, Scopus, Scopus: 1980 bis 2022
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Pages: - Volume / Issue: 56 Sequence Number: - Start / End Page: 657 - 687 Identifier: CoNE: https://gfzpublic.gfz-potsdam.de/cone/journals/resource/journals63