Deep mantle structure as a reference frame for movements in and on the Earth

Earth’s residual geoid is dominated by a degree-2 mode, with elevated regions above large low shear-wave velocity provinces on the core–mantle boundary beneath Africa and the Pacific. The edges of these deep mantle bodies, when projected radially to the Earth’s surface, correlate with the reconstruc...

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Bibliographic Details
Main Authors: Torsvik, Trond H., van der Voo, Rob, Doubrovine, Pavel V., Burke, Kevin, Steinberger, Bernhard, Ashwal, Lewis D., Trønnes, Reidar G., Webb, Susan J., Bull, Abigail L.
Format: Artigo
Language:Inglês
Published: National Academy of Sciences 2014
Subjects:
Physical Sciences
Online Access:https://ncbi.nlm.nih.gov/pmc/articles/PMC4066531/
https://ncbi.nlm.nih.gov/pubmed/24889632
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1318135111
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