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Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation

The sulfur cycle across the lithosphere and the role of this volatile element in the metasomatism of the mantle at ancient cratonic boundaries are poorly constrained. We address these knowledge gaps by tracking the journey of sulfur in the assembly of a Proterozoic supercontinent using mass independ...

Täydet tiedot

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Bibliografiset tiedot
Julkaisussa:Nat Commun
Päätekijät: LaFlamme, Crystal, Fiorentini, Marco L., Lindsay, Mark D., Bui, Thi Hao
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Nature Publishing Group UK 2018
Aiheet:
Linkit:https://ncbi.nlm.nih.gov/pmc/articles/PMC6197212/
https://ncbi.nlm.nih.gov/pubmed/30348984
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-06691-3
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