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Autor:
Giordano D.[1, 2, 3, Gonzalez-Garcia D.[1], Russell J.K.[5], Raneri S.[6], Bersani D.[7], Fornasini L.[7], Di Genova D.[8], Ferrando S.[1], Kaliwoda M.[4, Lottici P.P.[7], Smit M.[5], Dingwell D.B.[4]
Publikováno v:
Journal of Raman spectroscopy (Online) (2019): 1–17. doi:10.1002/jrs.5675
info:cnr-pdr/source/autori:Giordano D.[1,2,3,4], Gonzalez-Garcia D.[1], Russell J.K.[5], Raneri S.[6], Bersani D.[7], Fornasini L.[7], Di Genova D.[8], Ferrando S.[1], Kaliwoda M.[4,9], Lottici P.P.[7], Smit M.[5], Dingwell D.B.[4]/titolo:A calibrated database of Raman spectra for natural silicate glasses: implications for modelling melt physical properties/doi:10.1002%2Fjrs.5675/rivista:Journal of Raman spectroscopy (Online)/anno:2019/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume
info:cnr-pdr/source/autori:Giordano D.[1,2,3,4], Gonzalez-Garcia D.[1], Russell J.K.[5], Raneri S.[6], Bersani D.[7], Fornasini L.[7], Di Genova D.[8], Ferrando S.[1], Kaliwoda M.[4,9], Lottici P.P.[7], Smit M.[5], Dingwell D.B.[4]/titolo:A calibrated database of Raman spectra for natural silicate glasses: implications for modelling melt physical properties/doi:10.1002%2Fjrs.5675/rivista:Journal of Raman spectroscopy (Online)/anno:2019/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume
The physical properties of silicate melts are of critical importance for understanding magmatic and volcanic processes on Earth and other planets. Most physical properties of melts are, ultimately, a consequence of the structural organization of the