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Autor:
Maffeis A.[1], Ferrando S.[1], Connolly J.A.D.[2], Groppo C. [1, Frezzotti M.L.[4], Castelli D.[1]
Publikováno v:
Geochimica et cosmochimica acta 315 (2021): 207–229. doi:10.1016/j.gca.2021.08.044
info:cnr-pdr/source/autori:Maffeis A.[1], Ferrando S.[1], Connolly J.A.D.[2], Groppo C. [1,3], Frezzotti M.L.[4], Castelli D.[1]/titolo:Thermodynamic analysis of HP-UHP fluid inclusions: The solute load and chemistry of metamorphic fluids/doi:10.1016%2Fj.gca.2021.08.044/rivista:Geochimica et cosmochimica acta/anno:2021/pagina_da:207/pagina_a:229/intervallo_pagine:207–229/volume:315
info:cnr-pdr/source/autori:Maffeis A.[1], Ferrando S.[1], Connolly J.A.D.[2], Groppo C. [1,3], Frezzotti M.L.[4], Castelli D.[1]/titolo:Thermodynamic analysis of HP-UHP fluid inclusions: The solute load and chemistry of metamorphic fluids/doi:10.1016%2Fj.gca.2021.08.044/rivista:Geochimica et cosmochimica acta/anno:2021/pagina_da:207/pagina_a:229/intervallo_pagine:207–229/volume:315
Subduction fluids play a crucial role in regulating long-term chemical cycles. Their characterisation is essential to understand the processes responsible for metasomatism, oxidation and melting of the mantle wedge. Both direct (fluid inclusion studi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c908c1ba98b19209924ae8c3f5af81c
http://www.cnr.it/prodotto/i/460048
http://www.cnr.it/prodotto/i/460048