Heavy iron in large gem diamonds traces deep subduction of serpentinized ocean floor

Subducting tectonic plates carry water and other surficial components into Earth’s interior. Previous studies suggest that serpentinized peridotite is a key part of deep recycling, but this geochemical pathway has not been directly traced. Here, we report Fe-Ni–rich metallic inclusions in sublithosp...

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Detalles Bibliográficos
Autores principales: Smith, Evan M., Ni, Peng, Shirey, Steven B., Richardson, Stephen H., Wang, Wuyi, Shahar, Anat
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8011960/
https://www.ncbi.nlm.nih.gov/pubmed/33789901
http://dx.doi.org/10.1126/sciadv.abe9773

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8011960/
https://www.ncbi.nlm.nih.gov/pubmed/33789901
http://dx.doi.org/10.1126/sciadv.abe9773

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