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pro vyhledávání: '"Chakraborty S.[3]"'
Autor:
Halldórsson S.A.[1, Hilton D.R.[2], 1 Marshall E.W.[1], Ranta E.[1], Ingvason A.[1], Chakraborty S.[3], Robin J.G.[1], Rasmussen M.B.[1], Gibson S.A.[4], Ono S.[5], Scarsi P.[6], Abebe T.[6], Hopp J.[7], Barry P.H.[8], Castillo P.R.[2]
Publikováno v:
Chemical geology 589 (2022). doi:10.1016/j.chemgeo.2021.120682
info:cnr-pdr/source/autori:Halldórsson S.A.[1,2], Hilton D.R.[2],1 Marshall E.W.[1], Ranta E.[1], Ingvason A.[1], Chakraborty S.[3], Robin J.G.[1], Rasmussen M.B.[1], Gibson S.A.[4], Ono S.[5], Scarsi P.[6], Abebe T.[6], Hopp J.[7], Barry P.H.[8], Castillo P.R.[2]/titolo:Evidence from gas-rich ultramafic xenoliths for Superplume-derived recycled volatiles in the East African sub-continental mantle/doi:10.1016%2Fj.chemgeo.2021.120682/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:589
info:cnr-pdr/source/autori:Halldórsson S.A.[1,2], Hilton D.R.[2],1 Marshall E.W.[1], Ranta E.[1], Ingvason A.[1], Chakraborty S.[3], Robin J.G.[1], Rasmussen M.B.[1], Gibson S.A.[4], Ono S.[5], Scarsi P.[6], Abebe T.[6], Hopp J.[7], Barry P.H.[8], Castillo P.R.[2]/titolo:Evidence from gas-rich ultramafic xenoliths for Superplume-derived recycled volatiles in the East African sub-continental mantle/doi:10.1016%2Fj.chemgeo.2021.120682/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:589
Volatile-rich fluids are believed to play a key role in the metasomatic enrichment of the East African sub-continental lithospheric mantle (SCLM), but limited data is available on key volatile tracers such as CO2 and N2. We report new CO2 and N2 isot