Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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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 that argues for cold subduction as early as 1.8...
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Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
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TN_cdi_doaj_primary_oai_doaj_org_article_2d9e7d2339134f2691f5ad739f33e2f5
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_2d9e7d2339134f2691f5ad739f33e2f5
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/s41467-018-05140-5
