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Publikováno v:
Contributions to mineralogy and petrology 175 (2020). doi:10.1007/s00410-019-1651-x
info:cnr-pdr/source/autori:Campomenosi N.[1], Mazzucchelli M. L.[2], Mihailova B. D.[3], Angel R. J.[2,4], Alvaro M.[2]/titolo:Using polarized Raman spectroscopy to study the stress gradient in mineral systems with anomalous birefringence/doi:10.1007%2Fs00410-019-1651-x/rivista:Contributions to mineralogy and petrology/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:175
info:cnr-pdr/source/autori:Campomenosi N.[1], Mazzucchelli M. L.[2], Mihailova B. D.[3], Angel R. J.[2,4], Alvaro M.[2]/titolo:Using polarized Raman spectroscopy to study the stress gradient in mineral systems with anomalous birefringence/doi:10.1007%2Fs00410-019-1651-x/rivista:Contributions to mineralogy and petrology/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:175
Polarized Raman spectroscopy was applied to garnet hosts which exhibit anomalous birefringence around inclusions of zircon and quartz to elucidate the spatial distribution of the anisotropic strain fields in the vicinity of the host-inclusion boundar