Petrologic and geochemical investigation of carbonates in peridotite xenoliths from northeastern Tanzania
Primary carbonates in peridotite xenoliths from the East African Rift in northeastern Tanzania occur as intergranular patches with accessory minerals (olivine and spinel), as patches with accessory magmatic minerals (nepheline), and as round monomineralic inclusions in primary olivine grains.
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Veröffentlicht in: | Contributions to mineralogy and petrology 2000-08, Vol.139 (4), p.470-484 |
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Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | Primary carbonates in peridotite xenoliths from the East African Rift in northeastern Tanzania occur as intergranular patches with accessory minerals (olivine and spinel), as patches with accessory magmatic minerals (nepheline), and as round monomineralic inclusions in primary olivine grains. |
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ISSN: | 0010-7999 1432-0967 |
DOI: | 10.1007/s004100000144 |