Describing, characterizing and interpreting the nearly infinite variety of carbonate rocks are
conundrums–intricate and difficult problems having only conjectural answers–that have …

We have compiled stratigraphic ranges of genera of calcareous nannofossils, calcispheres,
planktonic foraminifers, larger benthic foraminifers, corals and rudists bivalves, and species …

La lámina cabalgante más antigua y septentrional de los Pirineos centrales (lámina
cabalgante de Bóixols) presenta una estructura de inversión de las cuencas extensivas …

The halokinetic structure of inverted salt‐related continental margins is frequently obliterated
by compressional overprinting. The Cretaceous Sopeira and Sant Gervàs subbasins of the …

Major changes occurred in Iberia during the Late Cretaceous. First, the cessation of the
previous rifting episode derived into generalized thermal subsidence in all basins, which in …

The attributes of a 'four-systems-tract'sequence are at times difficult to identify in outcrop-
scale carbonate successions. Poor exposure conditions, variable rates of sediment …

Shallow-marine carbonate deposition was widespread across the Arabian Plate during
much of the Late Permian–Mesozoic but was significantly interrupted by a major tectonically …

Cenomanian through Coniacian strata near the town of Sopeira in the south-central
Pyrenees (northern Spain) are composed of a variety of autochthonous and allochthonous …

Standard conceptual models propose that stratal patterns in carbonate depositional
sequences are controlled predominantly by relative sea-level oscillations, even during …

ABSTRACT The Aulet and Adons diapirs are exposures of Triassic Keuper evaporites in the
Ribagorça Basin in the south-central Pyrenees. The diapirs have been alternatively …