Petrographic, mineralogical and geochemical analyses of mixed siliciclastic-carbonate offshore deposits of the Pilmatué Member (Neuquén Basin) were carried out to define two scenarios for deposition: a confined ramp setting (CRS) and an open ramp setting (ORS). The CRS involves marly to carbonate-rich fine-grained mudstones, mostly laminated and non-bioturbated, enriched in redox proxies and depleted in rare earth elements (REE). The ORS comprises abundant siliciclastic-rich mudstones, mostly coarser-mudstones, depleted in redox proxies and with REE pattern similar to the PAAS. These variations are explained through fluctuations in carbonate productivity/terrigenous input, and changes in the circulation pattern of the basin. Within the CRS,...
The Vaca Muerta Formation (early Tithonian-early Valanginian) is a rhythmic succession of marls and ...
The Portezuelo Formation is part of a red bed sequence in the Neuquén Basin assigned to the Neuquén...
Mixed carbonate siliciclastic systems develop laterally and vertically complex sediment successions,...
The carbonate-mudstone-dominated Lower Cretaceous Agrio Formation is the youngest marine source rock...
Carbonate–siliciclastic high-frequency sequences are formed by reciprocal sedimentation. In silicicl...
Petrological and geochemical characteristics of sandstones and shales from the Carboniferous Cerro A...
region of the Neuqutn Basin (Argentina) accumulated in a hemipelagic outer amp/basin setting. The fo...
The interplay between carbonate production and siliciclastic input produces mixed systems that typic...
International audienceThe Agua de la Mula Member of the Agrio Formation in the Neuquén Basin, compri...
Most of the present knowledge of shallow-marine, mixed carbonate–siliciclastic systems relies on exa...
The Tithonian-Berriasian Vaca Muerta, Carrin Cura and Picun Leufu formations in the southern Neuquen...
Mixed siliciclastic-carbonate sediments in the distal settings of marine systems (i.e., offshore and...
La Manga Formation is a vast carbonate system developed in the Neuquén Basin. The age is based in am...
The Late Jurassic – Early Cretaceous slope and basin sediments of the Neuquén Basin, Argentina, cons...
The carbonatic sequence of the Calabozo Formation (Lower Callovian) developed in southwestern Gondwa...
The Vaca Muerta Formation (early Tithonian-early Valanginian) is a rhythmic succession of marls and ...
The Portezuelo Formation is part of a red bed sequence in the Neuquén Basin assigned to the Neuquén...
Mixed carbonate siliciclastic systems develop laterally and vertically complex sediment successions,...
The carbonate-mudstone-dominated Lower Cretaceous Agrio Formation is the youngest marine source rock...
Carbonate–siliciclastic high-frequency sequences are formed by reciprocal sedimentation. In silicicl...
Petrological and geochemical characteristics of sandstones and shales from the Carboniferous Cerro A...
region of the Neuqutn Basin (Argentina) accumulated in a hemipelagic outer amp/basin setting. The fo...
The interplay between carbonate production and siliciclastic input produces mixed systems that typic...
International audienceThe Agua de la Mula Member of the Agrio Formation in the Neuquén Basin, compri...
Most of the present knowledge of shallow-marine, mixed carbonate–siliciclastic systems relies on exa...
The Tithonian-Berriasian Vaca Muerta, Carrin Cura and Picun Leufu formations in the southern Neuquen...
Mixed siliciclastic-carbonate sediments in the distal settings of marine systems (i.e., offshore and...
La Manga Formation is a vast carbonate system developed in the Neuquén Basin. The age is based in am...
The Late Jurassic – Early Cretaceous slope and basin sediments of the Neuquén Basin, Argentina, cons...
The carbonatic sequence of the Calabozo Formation (Lower Callovian) developed in southwestern Gondwa...
The Vaca Muerta Formation (early Tithonian-early Valanginian) is a rhythmic succession of marls and ...
The Portezuelo Formation is part of a red bed sequence in the Neuquén Basin assigned to the Neuquén...
Mixed carbonate siliciclastic systems develop laterally and vertically complex sediment successions,...