Kinematics and dynamics of the East Pacific Rise linked to a stable, deep-mantle upwelling

Earth’s tectonic plates are generally considered to be driven largely by negative buoyancy associated with subduction of oceanic lithosphere. In this context, mid-ocean ridges (MORs) are passive plate boundaries whose divergence accommodates flow driven by subduction of oceanic slabs at trenches. We...

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Detalles Bibliográficos
Autores principales: Rowley, David B., Forte, Alessandro M., Rowan, Christopher J., Glišović, Petar, Moucha, Robert, Grand, Stephen P., Simmons, Nathan A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5182052/
https://www.ncbi.nlm.nih.gov/pubmed/28028535
http://dx.doi.org/10.1126/sciadv.1601107

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5182052/
https://www.ncbi.nlm.nih.gov/pubmed/28028535
http://dx.doi.org/10.1126/sciadv.1601107

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