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Cuantumul contributiilor – Filbuc Caa
Strong single-maximum crystal fabrics developed in ice undergoing shear with unconstrained normal deformation | Annals of Glaciology | Cambridge Core
Ice flow relations for stress and strain-rate components from combined shear and compression laboratory experiments | Journal of Glaciology | Cambridge Core
Origin of magmatic and tectonic fabrics in the Remal granite-gneiss, Singhbhum Craton, India | Geological Magazine | Cambridge Core