Origin of arc magmatic signature: A temperature-dependent process for trace element (re)-mobilization in subduction zones

Serpentinite is a major carrier of fluid-mobile elements in subduction zones, which influences the geochemical signature of arc magmatism (e.g. high abundances of Li, Ba, Sr, B, As, Mo and Pb). Based on results from Neoproterozoic serpentinites in the Arabian-Nubian Shield, we herein report the role...

Descripción completa

Detalles Bibliográficos
Autores principales: Gamal El Dien, Hamed, Li, Zheng-Xiang, Kil, Youngwoo, Abu-Alam, Tamer
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6506526/
https://www.ncbi.nlm.nih.gov/pubmed/31068627
http://dx.doi.org/10.1038/s41598-019-43605-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6506526/
https://www.ncbi.nlm.nih.gov/pubmed/31068627
http://dx.doi.org/10.1038/s41598-019-43605-9

Ejemplares similares