2019-09-242019-09-242019-07-19VENTURIERI, Enzo Maués. Glaciações paleozoicas no Gondwana, post-glacial-rebound e implicações geodinâmicas para o magmatismo do Grupo Serra Geral. Orientador: Roberto Vizeu Lima Pinheiro. 2019. 40 f. Trabalho de Curso (Bacharelado em Geologia) - Faculdade de Geologia, Instituto de Geociências, Universidade Federal do Pará, Belém, 2019. Disponível em: https://bdm.ufpa.br/jspui/handle/prefix/2110. Acesso em:.https://bdm.ufpa.br/jspui/handle/prefix/2110The event that formed the Igneous Province of Paraná corresponds to one of the major episodes of fissural magmatism occurred in a continental crust environment. The geological context of the region where it was placed records a sequence of peculiar geological events, such as Late Paleozoic glacial cycles that covered the paleocontinent Gondwana with extensive ice sheets. These series of glaciation cycles are recorded in the sedimentary sequences of the Itararé Group, contained in the Paraná Basin. The occurrence of glaciation cycles had an important effect on the lithospheric region that contained the Paraná Basin, since these ice addition and subtraction sequences had a direct effect on crustal isostasy, causing vertical movements to accommodate the accumulation of material and mass developed by the glaciers, a phenomena called lithostatic rebound. This same phenomenon can be observed in other regions of the planet, at different geological times. Due to this event reproduction, models used to study this phenomenon in one place, can be adapted and applied in other geological environments with occurrence of lithostatic rebound. This work sought to evaluate the possibility of replicability of the model proposed by Jull and McKenzie (1996), for the region of Iceland, which proved to be possible from adaptations of the model referring to the characteristics peculiar to the Paraná Basin region, as a resizing of the scale of application, volume of magma generated, time difference between the last glacial records and volcanism, crustal conditions related to thickness, viscoelasticity and temperature, as well as the height, extension and continuity of the ice column formed during glacial epochs.Acesso AbertoRebound litostáticoBacia do ParanáGrupo Serra GeralModelagemCNPQ::CIENCIAS EXATAS E DA TERRA::GEOCIENCIAS::GEOLOGIATrabalho de Curso - Graduação - Monografia