The isotropic and chemical constraints on the crustal evolution and source structure of Ferrar magmas, north Victoria Land, Antarctica

The isotropic and chemical constraints on the crustal evolution and source structure of Ferrar magmas, north Victoria Land, Antarctica

Isotropic and chemical compositions of the 177 Ma Kirkpatrick Basalt and Ferrar Dolerite from north Victoria Land, Antarctica, are examined in order to address the role of crustal assimilation and the characteristics of their mantle source.

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Bibliographische Detailangaben
Veröffentlicht in:Contributions to mineralogy and petrology 1995-09, Vol.121 (3), p.217
Hauptverfasser: Fleming, Thomas H, Foland, Kenneth A, Elliot, David H
Format: Artikel
Sprache:eng
Schlagworte:
Basalt
Chemicals
Evolution
Geology
Mineralogy
Petrology
Stone
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Beschreibung
Zusammenfassung:Isotropic and chemical compositions of the 177 Ma Kirkpatrick Basalt and Ferrar Dolerite from north Victoria Land, Antarctica, are examined in order to address the role of crustal assimilation and the characteristics of their mantle source.
ISSN:0010-7999
1432-0967