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Publikováno v:
Scientific Reports, Vol 9, Iss 1, Pp 1-7 (2019)
Scientific Reports
Scientific reports (Nature Publishing Group) 9 (2019). doi:10.1038/s41598-019-45031-3
info:cnr-pdr/source/autori:Dallai L.[1], Bianchini G.[2], Avanzinelli R.[3,4], Natali C.[2,3], Conticelli S. [3,4,5]/titolo:Heavy oxygen recycled into the lithospheric mantle/doi:10.1038%2Fs41598-019-45031-3/rivista:Scientific reports (Nature Publishing Group)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:9
Scientific Reports
Scientific reports (Nature Publishing Group) 9 (2019). doi:10.1038/s41598-019-45031-3
info:cnr-pdr/source/autori:Dallai L.[1], Bianchini G.[2], Avanzinelli R.[3,4], Natali C.[2,3], Conticelli S. [3,4,5]/titolo:Heavy oxygen recycled into the lithospheric mantle/doi:10.1038%2Fs41598-019-45031-3/rivista:Scientific reports (Nature Publishing Group)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:9
Magmas in volcanic arcs have geochemical and isotopic signatures that can be related to mantle metasomatism due to fluids and melts released by the down-going oceanic crust and overlying sediments, which modify the chemistry and mineralogy of the man