Lasting mantle scars lead to perennial plate tectonics

Mid-ocean ridges, transform faults, subduction and continental collisions form the conventional theory of plate tectonics to explain non-rigid behaviour at plate boundaries. However, the theory does not explain directly the processes involved in intraplate deformation and seismicity. Recently, damag...

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Detalles Bibliográficos
Autores principales: Heron, Philip J., Pysklywec, Russell N., Stephenson, Randell
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4906409/
https://www.ncbi.nlm.nih.gov/pubmed/27282541
http://dx.doi.org/10.1038/ncomms11834

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4906409/
https://www.ncbi.nlm.nih.gov/pubmed/27282541
http://dx.doi.org/10.1038/ncomms11834

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