Continental crust beneath southeast Iceland

The magmatic activity (0–16 Ma) in Iceland is linked to a deep mantle plume that has been active for the past 62 My. Icelandic and northeast Atlantic basalts contain variable proportions of two enriched components, interpreted as recycled oceanic crust supplied by the plume, and subcontinental litho...

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Detaylı Bibliyografya
Yayımlandı:Proc Natl Acad Sci U S A
Asıl Yazarlar: Torsvik, Trond H., Amundsen, Hans E. F., Trønnes, Reidar G., Doubrovine, Pavel V., Gaina, Carmen, Kusznir, Nick J., Steinberger, Bernhard, Corfu, Fernando, Ashwal, Lewis D., Griffin, William L., Werner, Stephanie C., Jamtveit, Bjørn
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: National Academy of Sciences 2015
Konular:
PNAS Plus
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC4403175/
https://ncbi.nlm.nih.gov/pubmed/25825769
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1423099112
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