Garnet growth and mineral geochronology constrains the diachronous Neoproterozoic convergent evolution of the southern Dom Feliciano Belt, Uruguay
The Dom Feliciano Belt of southern Brazil and Uruguay represents part of a larger Neoproterozoic orogenic system formed during the amalgamation of Western Gondwana. The hinterland and foreland domains in parts of the belt preserve deformation structures and metamorphic assemblages that developed dur...
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| Other Authors: | , , , |
| Format: | article |
| Language: | English |
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2023
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| Online Access: | https://hdl.handle.net/20.500.12008/42364 |
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