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  Partition Coefficients of Trace Elements Between Carbonates and Melt and Suprasolidus Phase Relation of Ca-Mg-Carbonates at 6 Gpa

Sieber, M., Wilke, F., Koch-Müller, M. (2020): Partition Coefficients of Trace Elements Between Carbonates and Melt and Suprasolidus Phase Relation of Ca-Mg-Carbonates at 6 Gpa. - American Mineralogist, 105, 6, 922-933.
https://doi.org/10.2138/am-2020-7098

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 Creators:
Sieber, Melanie1, Author              
Wilke, F.2, Author              
Koch-Müller, M.1, Author              
Affiliations:
13.6 Chemistry and Physics of Earth Materials, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146036              
23.1 Inorganic and Isotope Geochemistry, 3.0 Geochemistry, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146040              

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Free keywords: FINAL DRAFT VORHANDEN
 Abstract: By performing high pressure and temperature experiments, this study clarifies the suprasolidus phase relations of the nominally anhydrous Ca-Mg-CO3 system at 6 GPa showing that Ca-Mg-carbonates will (partially) melt for temperatures above ~1300 ℃. Further, partition coefficients for Li, Na, K, Mn, Fe, Sr, Ba, Pb, Nb, Y and rare earth elements between dolomite and dolomitic melt, Ca-magnesite and dolomitic melt and magnesite and dolomitic melt are established.

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Language(s): eng - English
 Dates: 2020-02-032020
 Publication Status: Finally published
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 Rev. Type: -
 Identifiers: DOI: 10.2138/am-2020-7098
GFZPOF: p3 PT2 Plate Boundary Systems
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Title: American Mineralogist
Source Genre: Journal, SCI, Scopus
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Pages: - Volume / Issue: 105 (6) Sequence Number: - Start / End Page: 922 - 933 Identifier: CoNE: https://gfzpublic.gfz-potsdam.de/cone/journals/resource/journals22
Publisher: Mineralogical Society of America (MSA)