Geochemical signature of the Egersund basaltic dyke swarm, SW Norway, in the context of late-Neoproterozoic opening of the Iapetus Ocean
Author:
Publisher
Informa UK Limited
Subject
Geology
Link
http://www.tandfonline.com/doi/pdf/10.1080/002919699433825
Reference63 articles.
1. How deep do common basaltic magmas form and differentiate?
2. Radiogenic isotope systematics of the Herefoss granite, South Norway: an indicator of Sveconorwegian (Grenvillian) crustal evolution in the Baltic Shield
3. The sublithospheric mantle as the source of continental flood basalts; the case against the continental lithosphere and plume head reservoirs
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