Integration of regional stratigraphic relationships with data on sediment accumulation,
provenance, paleodrainage, and deformation timing enables a reconstruction of Mesozoic …

Abstract The Triassic–Jurassic transition is characterized by the end-Triassic mass extinction
approximately synchronous with the onset of emplacement of the Central Atlantic Magmatic …

Construction of the Andes has been governed largely by fluctuating contractional, neutral,
and extensional tectonic regimes during differing degrees of mechanical coupling along the …

Provenance of detrital sediments of the Neuquén Basin in Central Argentina was
investigated using U–Pb and Lu–Hf isotopic composition of zircon grains in order to …

El Grupo Neuquén conforma una sucesión de depósitos continentales de origen fluvial,
eólico y lacustre somero, desarrollado en la Cuenca Neuquina entre el Cenomaniano …

Abstract The Vaca Muerta Formation (early Tithonian–early Valanginian) is a rhythmic
succession of marls and limestones, cropping out in the Neuquén Basin, west-central …

The temporal transition from backarc extension to retroarc shortening is a fundamental
process in the evolution of many Andean-type convergent margins. This switch in tectonic …

We investigate the use of Hg as a proxy for volcanism by studying four distal and two
proximal sections in relation to the Deccan volcanic center, straddling the Cretaceous …

Abstract The Pliensbachian–Toarcian boundary interval is characterized by a~ 3‰ negative
carbon-isotope excursion (CIE) in organic and inorganic marine and terrestrial archives from …

Numerous sedimentary basins in the world host voluminous igneous sill-complexes, ie
stacking of sills that are emplaced in different levels of the sedimentary sequence. When sills …