Carbonate-bearing mantle peridotite xenoliths from Spitsbergen: phase relationships, mineral compositions and trace-element residence

Carbonates of mantle origin have been found in xenoliths from Quaternary basaltic volcanoes in northwest Spitsbergen Norway. The carbonates range from dolomite to Mg-bearing calcite and have high Mg-numbers.

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Veröffentlicht in:Contributions to mineralogy and petrology 1996-11, Vol.125 (4), p.375-392
Hauptverfasser: Ionov, D. A., O'Reilly, Suzanne Y., Genshaft, Yuri S., Kopylova, Maya G.
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Sprache:eng
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Zusammenfassung:Carbonates of mantle origin have been found in xenoliths from Quaternary basaltic volcanoes in northwest Spitsbergen Norway. The carbonates range from dolomite to Mg-bearing calcite and have high Mg-numbers.
ISSN:0010-7999
1432-0967
DOI:10.1007/s004100050229