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...

ver descrição completa

Na minha lista:
Detalhes bibliográficos
Publicado no: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
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2015
Assuntos:
PNAS Plus
Acesso em linha: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
Tags: Adicionar Tag
Sem tags, seja o primeiro a adicionar uma tag!

Registos relacionados