Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
The onset of modern-style plate tectonics remains under debate. Here, Xu et al. report a cold thermal-gradient recorded in an eclogite xenolith in Paleoproterozoic carbonatite from orogen, and propose that modern-style subduction has operated since at least the Paleoproterozoic.
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Auteurs principaux: | , , , , , , , , , , |
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Format: | article |
Langue: | EN |
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Nature Portfolio
2018
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Accès en ligne: | https://doaj.org/article/2d9e7d2339134f2691f5ad739f33e2f5 |
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