Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry

The evolution of the planetary interior during plate tectonics is controlled by slow convection within the mantle. Global-scale geochemical differences across the upper mantle are known, but how they are preserved during convection has not been adequately explained. We demonstrate that the geographi...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Sci Rep
Prif Awduron: Barry, T. L., Davies, J. H., Wolstencroft, M., Millar, I. L., Zhao, Z., Jian, P., Safonova, I., Price, M.
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Nature Publishing Group UK 2017
Pynciau:
Article
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC5431867/
https://ncbi.nlm.nih.gov/pubmed/28500352
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-01816-y
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