Magma transport in sheet intrusions of the Alnö carbonatite complex, central Sweden

Magma transport through the Earth’s crust occurs dominantly via sheet intrusions, such as dykes and cone-sheets, and is fundamental to crustal evolution, volcanic eruptions and geochemical element cycling. However, reliable methods to reconstruct flow direction in solidified sheet intrusions have pr...

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Detalles Bibliográficos
Autores principales: Andersson, Magnus, Almqvist, Bjarne S. G., Burchardt, Steffi, Troll, Valentin R., Malehmir, Alireza, Snowball, Ian, Kübler, Lutz
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4901264/
https://www.ncbi.nlm.nih.gov/pubmed/27282420
http://dx.doi.org/10.1038/srep27635

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4901264/
https://www.ncbi.nlm.nih.gov/pubmed/27282420
http://dx.doi.org/10.1038/srep27635

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