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...

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Detalles Bibliográficos
Autores principales: LaFlamme, Crystal, Fiorentini, Marco L., Lindsay, Mark D., Bui, Thi Hao
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/PMC6197212/
https://www.ncbi.nlm.nih.gov/pubmed/30348984
http://dx.doi.org/10.1038/s41467-018-06691-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6197212/
https://www.ncbi.nlm.nih.gov/pubmed/30348984
http://dx.doi.org/10.1038/s41467-018-06691-3

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