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Palaeoproterozoic assembly of the São Francisco craton, SE Brazil: New insights from U-Pb titanite and monazite dating
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文摘
Southern São Francisco craton titanite and monazite resetting between 2080 and 1940 Ma. Syn-collisional metamorphism between 2100 and 2070 Ma. Final closure of the Minas basin in the 2100–2070 Ma interval. Dome-and-keel structure generated by orogenic collapse at ca. 2070–2050 Ma. Slow cooling lasted until ca.1940 Ma.

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