Pelocorrientes de las Eoleanitas Mesozoicas en el Norte Uruguayo
DOI:
https://doi.org/10.5902/2179460X26197Abstract
Paleocurrents of the Triassic-Jurasic eoleanites from the final units of the Cuenca deI Paraná Gondwanic sedimentation has been characterized as result of 1/100.000 survey at the Uruguayan frontier belt, delimited by Rivera City, Capón Alto Place, and 27 road.
Cuchilla Ombú formation, possible aged Medium Triassic, presents SE mean orientation; eolic facies of Tacuarembó formation has principal component to ENE, and a great dominance of the NE direction at the upper Formation Rivera.
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FERRANDO. L.A. (1966) Guia Excursión a los depósitos Gondwánicos de Tacuarembó Proyecto 193 Silúrico-Devónico de América Latina. IV Reunión Técnica. Tacuarembó, Uruguay.
FERRANDO, L.A. y R.R. ANDREIS (1986) Nueva estratigrafía en el Gondwana de Uruguay. 1. Congreso Latinoamericano de Hidrocarburos. ARPEL I: 295-323, Buenos Aires, Argentina.
FERRANDO, L.A. R.R. ANDREIS y J .R. MONTAÑA (1987) Estratigrafía del Triásico-Jurásico uruguayo en Ia Cuenca de Paraná. Atas do III Simpósio Sul-Brasileiro de Geologia, 1:373-378, Curitiba, Brasil.
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