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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Detalles Bibliográficos
Autores principales: Xu, Cheng, Kynický, Jindřich, Song, Wenlei, Tao, Renbiao, Lü, Zeng, Li, Yunxiu, Yang, Yueheng, Pohanka, Miroslav, Galiova, Michaela V., Zhang, Lifei, Fei, Yingwei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6050299/
https://www.ncbi.nlm.nih.gov/pubmed/30018373
http://dx.doi.org/10.1038/s41467-018-05140-5

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6050299/
https://www.ncbi.nlm.nih.gov/pubmed/30018373
http://dx.doi.org/10.1038/s41467-018-05140-5

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