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On the magmatic evolution of the alkaline igneous province of South Greenland

Name: On the magmatic evolution of the alkaline igneous province of South Greenland
Creator: H Sørensen
Keywords: 13. Climate action

descriptionPublicationkeyboard_double_arrow_right Article , Other literature type 01 Jan 1966Publisher:Geological Survey of Denmark and GreenlandJournal:Rapport Grønlands Geologiske Undersøgelse, volume 7, pages 1-19 (issn: 0418-6559, eissn: 2597-2944,

Authors: H Sørensen;

doi: 10.34194/rapggu.v7.7132

On the magmatic evolution of the alkaline igneous province of South Greenland

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Abstract

In 1938 E. Wegmann divided the rocks of southern Greenland into and old basement and a younger formation. The basement consists of the remains of a mountain chain for which Wegmann introduced the name the Ketilides. The younger rocks, which are separated from the Ketilidian orogeny by a long period of denudation, were grouped in the Gardar formation. The Gardar "formation" comprises supracrustal rocks, a great number of dykes and a limited number of plutonic bodies. In this article an outline of the geology and the magmatic evolution of the Gardar province will be given.

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