2020
DOI: 10.1016/j.precamres.2020.105963
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Nd-Sr-Hf isotopes and U-Pb ages of mesoproterozoic Três Estradas Alkaline-Carbonatite Complex, Brazil: Implications for Sul-Riograndense Shield evolution and rodinia break-up

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Cited by 4 publications
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“…Granulitic Complex interpreted as a 2.4 Ga magmatic arc (Girelli et al, 2018;Nardi & Hartmann, 1979) make up the majority of the Río de la Plata Craton. Subordinately in the craton, Mesoproterozoic rocks (Três Estradas Carbonatite Complex;Monteiro et al, 2020) and several Neoproterozoic units occur (Laux, 2017). The remaining units of the Sul-rio-grandense Shield belong to the Neoproterozoic DFB, which is separated from the cratonic area by the geophysical discontinuity known as the Ibaré Lineament or São Gabriel Suture (Fernandes et al, 1995b;Hartmann et al, 2016).…”
Section: Rocks Belonging To the Palaeoproterozoic Santa Maria Chicomentioning
confidence: 99%
“…Granulitic Complex interpreted as a 2.4 Ga magmatic arc (Girelli et al, 2018;Nardi & Hartmann, 1979) make up the majority of the Río de la Plata Craton. Subordinately in the craton, Mesoproterozoic rocks (Três Estradas Carbonatite Complex;Monteiro et al, 2020) and several Neoproterozoic units occur (Laux, 2017). The remaining units of the Sul-rio-grandense Shield belong to the Neoproterozoic DFB, which is separated from the cratonic area by the geophysical discontinuity known as the Ibaré Lineament or São Gabriel Suture (Fernandes et al, 1995b;Hartmann et al, 2016).…”
Section: Rocks Belonging To the Palaeoproterozoic Santa Maria Chicomentioning
confidence: 99%