Abstract The Neuquén Basin, located at the foothills of the Central Andes of Argentina, with
superb and extended exposures, is a natural laboratory. It is important not only for its …

Cooling subvolcanic igneous intrusions are known to have a tremendous impact on fluid
flow in the shallow Earth's crust. However, the long-term post-cooling legacy of subvolcanic …

Volcanic plumbing systems emplaced in sedimentary basins may exert significant
mechanical and thermal effects on petroleum systems. The last decade of research has …

This contribution presents a detailed geological study of a well-exposed igneous petroleum
system at Sierra de Cara Cura, Neuquén Basin, Argentina, which consists of sills, dykes …

Laccolith emplacement and growth are controlled by doming of overburden rocks.
Understanding the mechanics and structural evolution of laccolith-induced doming is …

Fibrous calcite bed‐parallel veins (BPVs) are a typical feature of the Upper Jurassic–Lower
Cretaceous Vaca Muerta Formation in the subsurface of the Neuquén Basin (Argentina) …

Organic carbon-bearing mudstone units of variable lithologies exhibit complex internal
heterogeneities in total organic carbon (TOC) enrichment and mineralogy related to …

Abstract The Agrio Fold and Thrust Belt (FTB), situated in the Southern Central Andes at 37–
39° S, underwent two phases of contractional deformation: Late Cretaceous‐Eocene and …

Abstract The Neuquén Basin is a major Mesozoic sedimentary depocentre located in the
retroarc foreland of the Argentinian Andes. The basin hosts world renowned inversion …

The 50 m-thick Berriasian organic-rich interval (BORI) of the Vaca Muerta Formation
(Neuquén Basin, Argentina) represents one of the most attractive stratigraphic intervals for …