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Continuous plate subduction marked by the rise of alkali magmatism 2.1 billion years ago
Over the Earth’s evolutionary history, the style of plate subduction has evolved through time due to the secular cooling of the mantle. While continuous subduction is a typical feature of modern plate tectonics, a stagnant-lid tectonic regime with localized episodic subduction likely characterized t...
| Autores principales: | , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2019
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6667441/ https://www.ncbi.nlm.nih.gov/pubmed/31363091 http://dx.doi.org/10.1038/s41467-019-11329-z |