Depletion of the upper mantle by convergent tectonics in the Early Earth
Abstract Partial melting of mantle peridotites at spreading ridges is a continuous global process that forms the oceanic crust and refractory, positively buoyant residues (melt-depleted mantle peridotites). In the modern Earth, these rocks enter subduction zones as part of the oceanic lithosphere. H...
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| Autores principales: | , , , |
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| Formato: | article |
| Lenguaje: | EN |
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Nature Portfolio
2021
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| Acceso en línea: | https://doaj.org/article/a042816e5bdc40dfb20898a07e572ccd |
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