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PreviewIssue DateTitleAuthor(s)
2021Th‐U powered metamorphism: thermal consequences of a chemical hotspotDe Vries Van Leeuwen, A.T.; Hand, M.; Morrissey, L.J.; Raimondo, T.
2020Contrasting P-T-t paths reveal a metamorphic discontinuity in the New Quebec Orogen: insights into Paleoproterozoic orogenic processesGodet, A.; Guilmette, C.; Labrousse, L.; Smit, M.A.; Davis, D.W.; Raimondo, T.; Vanier, M.A.; Charette, B.; Lafrance, I.
2020Experimental alteration of monazite in granitic melt: Variable U–Th–Pb and REE mobility during melt-mediated coupled dissolution-precipitationVarga, J.; Raimondo, T.; Daczko, N.R.; Adam, J.
2020Melt-present shear zones enable intracontinental orogenesisPiazolo, S.; Daczko, N.R.; Silva, D.; Raimondo, T.
2021Garnet as a monitor for melt‐rock interaction: textural, mineralogical and compositional evidence of partial melting and melt‐driven metasomatismGoncalves, P.; Raimondo, T.; Paquette, J.; de Souza, J.S.
2022Prolonged high thermal gradient metamorphism in the Curnamona Province, south-central Australia, during the latter stages of Nuna assemblyDe Vries Van Leeuwen, A.T.; Morrissey, L.J.; Raimondo, T.; Hand, M.
2022Pressure-temperature-time constraints on gneiss dome formation in an intracontinental orogenVarga, J.; Raimondo, T.; Morrissey, L.; Kelsey, D.E.; Hand, M.
2022Glimmerite: A product of melt-rock interaction within a crustal-scale high-strain zoneSilva, D.; Daczko, N.R.; Piazolo, S.; Raimondo, T.
2021PetroChron Antarctica: a geological database for interdisciplinary useSanchez, G.; Halpin, J.A.; Gard, M.; Hasterok, D.; Stål, T.; Raimondo, T.; Peters, S.; Burton‐Johnson, A.