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- W4234287768 abstract "An approach, to the structural and geológical evolution of the Southern orogenic Brasiliano limit in Uruguay is presented. As a consequence of sinistral shearing during the Late Brasiliano, the dextral wrench fault (Sarandí del Yi – Aº Solís Grande) of probably pre-Brasiliano age, is reactivated with intrusion of syn-transcurrent granites. Post-uplift processes, through alkaline and slightly oversaturated magmatism associated with molassic sediments, are observed." @default.
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- W4234287768 date "1993-09-01" @default.
- W4234287768 modified "2023-10-06" @default.
- W4234287768 title "GEOLOGIA Y ASPECTOS ESTRUCTURALES DEL BORDE OROGÉNICO EN EL EXTREMO SUR DEL CINTURON DON FELICIANO" @default.
- W4234287768 doi "https://doi.org/10.25249/0375-7536.1993233296300" @default.
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