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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| Altri autori: | , , , |
| Natura: | article |
| Lingua: | inglese |
| Pubblicazione: |
2023
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| Accesso online: | https://hdl.handle.net/20.500.12008/42364 |
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