2020
DOI: 10.1016/j.gsf.2020.01.015
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Neoarchean and Rhyacian TTG-Sanukitoid suites in the southern São Francisco Paleocontinent, Brazil: Evidence for diachronous change towards modern tectonics

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Cited by 53 publications
(26 citation statements)
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“…Sample 66B is a tholeiitic metabasic rock crystallized at 2710 ± 32 Ma and metamorphosed under granulite facies metamorphism at 2067 ± 82 Ma (Bruno et. al., 2020).…”
Section: Neoarchean Piedade Microcontinentmentioning
confidence: 99%
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“…Sample 66B is a tholeiitic metabasic rock crystallized at 2710 ± 32 Ma and metamorphosed under granulite facies metamorphism at 2067 ± 82 Ma (Bruno et. al., 2020).…”
Section: Neoarchean Piedade Microcontinentmentioning
confidence: 99%
“…Sample 08, a hornblende biotite gneiss of the sanukitoid compositional group displays prismatic, euhedral to subhedral zircon grains with fine igneous oscillatory zoning in the cores surrounded by homogeneous bright rims with crystallization age defined by an upper intercept of 2168 ± 21 Ma and metamorphic overprint defined by a lower intercept of 584 ± 14 Ma (Bruno et. al., 2020).…”
Section: Mantiqueira Magmatic Arcmentioning
confidence: 99%
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