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Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
The absence of low-thermal gradients in old metamorphic rocks (<350 °C GPa(−1)) has been used to argue for a fundamental change in the style of plate tectonics during the Neoproterozoic Era. Here, we report data from an eclogite xenolith in Paleoproterozoic carbonatite in the North China craton t...
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| Publicado no: | Nat Commun |
|---|---|
| Main Authors: | , , , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6050299/ https://ncbi.nlm.nih.gov/pubmed/30018373 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05140-5 |
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