|
|
|
|
|
Diego Alejandro Kietzmann,Verónica Vanesa Vennari
Pág. 41 - 65
The Vaca Muerta Formation in the Cerro Domuyo area shows an interesting intercalationof facies with opposite paleocurrents. The unit is represented by outer ramp to basinal facies with a westward directionof progradation. However, in its middle section, ...
ver más
|
|
|
|
|
|
|
|
|
|
|
Lucia Sagripanti,German Bottesi,Diego Kietzmann,Andres Folguera,Victor Ramos
Pág. 201 - 219
The orogenic front at 37ºS has been mainly formed through at least two contraccional stages, as inferred from the exhumed major angular unconformities at the Late Eocene and the Late Miocene times respectively. A Late Cretaceous event is restricted to th...
ver más
|
|
|
|
|
|