Chemical and physical evolution of the ‘lower layered sequence’ from the nepheline syenitic Ilímaussaq intrusion, South Greenland: Implications for the origin of magmatic layering in peralkaline felsic liquids-Reference-Cited by-同舟云学术

Chemical and physical evolution of the ‘lower layered sequence’ from the nepheline syenitic Ilímaussaq intrusion, South Greenland: Implications for the origin of magmatic layering in peralkaline felsic liquids

Published:2008-12 Issue:3-4 Volume:106 Page:280-296
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Pfaff Katharina,Krumrei Thomas,Marks Michael,Wenzel Thomas,Rudolf Tina,Markl Gregor

Funder

Deutsche Forschungsgemeinschaft

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference72 articles.

1. Zr–Y–U stratigraphy of the kakortokite–lujavrite sequence, southern Ilímaussaq intrusion;Andersen;Rapport Grønlands Geologiske Undersøgelse,1981

2. A geological section through the southern part of the Ilímaussaq intrusion;Andersen;Rapport Grønlands Geologiske Undersøgelse,1981

3. Quantitative elemental analysis of individual microparticles with electron beam instruments;Armstrong,1991

4. Geochemical overview of the Ilímaussaq alkaline complex, South Greenland;Bailey;Bulletin of the geological Survey of Greenland,2001

5. On the origin of microrhythmic layering in arfvedsonite lujavrite from the Ilímaussaq alkaline complex, South Greenland;Bailey;Lithos,2006

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