The Tithonian-Berriasian Vaca Muerta, Carrin Cura and Picun Leufu formations in the southern Neuquen Basin were deposited on a tidally dominated, mixed carbonate-siliciclastic ramp. Basinal, outer, middle, shallow and back ramp facies associations are recognized and a sequence stratigraphic analysis reveals that the ramp record consists of three shallowing-upwards sequences (Ti1, Ti2 and Ti3) set within a lower-order progradational cycle. A higher order of cyclicity is superimposed on to the middle (Ti2) sequence. The majority of the ramp facies belong to the transgressive and highstand systems tracts; however, at the base of Ti2, a lowstand systems tract is identified, characterized by a basal unconformity and an abrupt basinward shift of ...
Petrographic, mineralogical and geochemical analyses of mixed siliciclastic-carbonate offshore depos...
The area is located in west central Argentina, east of the Andes. It was a Mesozoic backarc basin wh...
The Vaca Muerta-Quintuco system (uppermost lower Tithonian-lower Valanginian) is a thick shallowing-...
The Vaca Muerta Formation (early Tithonian-early Valanginian) is a rhythmic succession of marls and ...
Mixed carbonate siliciclastic systems develop laterally and vertically complex sediment successions,...
The Vaca Muerta Formation (early Tithonian–early Valanginian) is a rhythmic succession of marls and ...
ACLInternational audienceThe Tithonian-Berriasian interval in the southern part of the Neuquén Basin...
The Vaca Muerta Formation (early Tithonian–early Valanginian) is a rhythmic succession of marls and ...
Carbonate–siliciclastic high-frequency sequences are formed by reciprocal sedimentation. In silicicl...
La Manga Formation is a vast carbonate system developed in the Neuquén Basin. The age is based in am...
The interplay between carbonate production and siliciclastic input produces mixed systems that typic...
Detailed sedimentological, sequence stratigraphical and cyclostratigraphical analyses have been made...
The La Manga Formation consists of marine carbonates and represents most of the sedimentary record o...
The outcrops of the Oxfordian La Manga Formation at Bardas Blancas, Neuquén Basin, west-central Arge...
The Late Jurassic – Early Cretaceous slope and basin sediments of the Neuquén Basin, Argentina, cons...
Petrographic, mineralogical and geochemical analyses of mixed siliciclastic-carbonate offshore depos...
The area is located in west central Argentina, east of the Andes. It was a Mesozoic backarc basin wh...
The Vaca Muerta-Quintuco system (uppermost lower Tithonian-lower Valanginian) is a thick shallowing-...
The Vaca Muerta Formation (early Tithonian-early Valanginian) is a rhythmic succession of marls and ...
Mixed carbonate siliciclastic systems develop laterally and vertically complex sediment successions,...
The Vaca Muerta Formation (early Tithonian–early Valanginian) is a rhythmic succession of marls and ...
ACLInternational audienceThe Tithonian-Berriasian interval in the southern part of the Neuquén Basin...
The Vaca Muerta Formation (early Tithonian–early Valanginian) is a rhythmic succession of marls and ...
Carbonate–siliciclastic high-frequency sequences are formed by reciprocal sedimentation. In silicicl...
La Manga Formation is a vast carbonate system developed in the Neuquén Basin. The age is based in am...
The interplay between carbonate production and siliciclastic input produces mixed systems that typic...
Detailed sedimentological, sequence stratigraphical and cyclostratigraphical analyses have been made...
The La Manga Formation consists of marine carbonates and represents most of the sedimentary record o...
The outcrops of the Oxfordian La Manga Formation at Bardas Blancas, Neuquén Basin, west-central Arge...
The Late Jurassic – Early Cretaceous slope and basin sediments of the Neuquén Basin, Argentina, cons...
Petrographic, mineralogical and geochemical analyses of mixed siliciclastic-carbonate offshore depos...
The area is located in west central Argentina, east of the Andes. It was a Mesozoic backarc basin wh...
The Vaca Muerta-Quintuco system (uppermost lower Tithonian-lower Valanginian) is a thick shallowing-...