Birth of an oceanic spreading center at a magma-poor rift system

Oceanic crust is continuously created at mid-oceanic ridges and seafloor spreading represents one of the main processes of plate tectonics. However, if oceanic crust architecture, composition and formation at present-day oceanic ridges are largely described, the processes governing the birth of a sp...

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Detalles Bibliográficos
Autores principales: Gillard, Morgane, Sauter, Daniel, Tugend, Julie, Tomasi, Simon, Epin, Marie-Eva, Manatschal, Gianreto
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5678130/
https://www.ncbi.nlm.nih.gov/pubmed/29118393
http://dx.doi.org/10.1038/s41598-017-15522-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5678130/
https://www.ncbi.nlm.nih.gov/pubmed/29118393
http://dx.doi.org/10.1038/s41598-017-15522-2

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