• Pereira, I., Dias, R., Bento dos Santos, T., Mata, J., 2017. Exhumation of a migmatite complex along a transpressive shear zone: inferences from the Variscan Juzbado-Penalva do Castelo Shear Zone (Central Iberian Zone). Journal of the Geological Society, 174, 6, 1004-1018 (doi: 10.1144/jgs2016-159).
• Jesus, A.P., Mateus, A., Munhá, J.M., Tassinari, C.C.G., Bento dos Santos, T., Benoit, M., 2016. Evidence for underplating in the genesis of the Variscan synorogenic Beja Layered Gabbroic Sequence (Portugal) and related mesocratic rocks. Tectonophysics, 683, 148-171 (doi: 10.1016/j.tecto.2016.06.001).
• Bento dos Santos, T., Tassinari, C.C.G., Fonseca, P.E., 2015. Diachronic collision, slab break-off and long-term high thermal flux in the Brasiliano - Pan-African orogeny: Implications for the geodynamic evolution of the Mantiqueira Province. Precambrian Research, 260, 1-22 (doi: 10.1016/j.precamres.2014.12.018).
• Bento dos Santos, T., Tassinari, C.C.G., Fonseca, P.E., 2014. Garnet-biotite diffusion mechanisms in granulites from Ribeira Fold Belt (SE Brazil): Understanding and constraining petrological cooling rates in complex high-grade orogenic belts. Journal of South American Earth Sciences, 56, 128-138 (doi: 10.1016/j.jsames.2014.09.003).
• Bento dos Santos, T., Munhá, J.M.U., Tassinari, C.C.G., Fonseca, P.E., Dias Neto, C.M., 2010. Thermochronology of central Ribeira Fold Belt, SE Brazil: Petrological and geochronological evidence for high-temperature maintenance during Western Gondwana amalgamation. Precambrian Research, 180, 3-4, 285-298 (doi: 10.1016/j.precamres.2010.05.002).

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