Mantle heterogeneity caused by trapped water in the Southwest Basin of the South China Sea

Water is the most common volatile component inside the Earth. A substantial amount of water can be carried down to the interior of the Earth by subducting plates. However, how the subducted water evolves after the subducting slab breaks off remains poorly understood. Here we use the data from a pass...

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Detalles Bibliográficos
Autores principales: Tian, Jinyu, Ma, Zhitu, Lin, Jian, Xu, Min, Yu, Xun, Le, Ba Manh, Zhang, Xubo, Zhang, Fan, Guo, Laiyin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10175291/
https://www.ncbi.nlm.nih.gov/pubmed/37169745
http://dx.doi.org/10.1038/s41467-023-38385-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10175291/
https://www.ncbi.nlm.nih.gov/pubmed/37169745
http://dx.doi.org/10.1038/s41467-023-38385-w

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