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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Bibliografske podrobnosti
izdano v:Proc Natl Acad Sci U S A
Main Authors: 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
Format: Artigo
Jezik:Inglês
Izdano: National Academy of Sciences 2015
Teme:
PNAS Plus
Online dostop: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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