Unconformities in foreland basins may be generated by tectonic processes that operate in
the basin, the adjacent fold–thrust belt or the broader convergent margin. Foreland basin …

Subduction of bathymetric anomalies (eg, an active ridge) can alter the morphology of
subducted slabs and their coupling to surface processes. A natural laboratory to study these …

This paper characterizes the depth of the Mohorovičić discontinuity and the crustal structure
in the foreland of the Central Andes, Santiago del Estero, Argentina, using gravimetric …

Sedimentary basins result from a complex interaction between mantle, crustal and surficial
erosional-driven processes, which act at different time and spatial scales. While shortening …

We present a new tectonic plate reconstruction that suggests substantial revisions to events
associated with development of the Peruvian flat slab and resolves several long-standing …

Kinematic restorations in fold and thrust belts, which are a valuable tool for studying the
deformational history of fold and thrust belts, have been poorly used to understand erosion …

Paleoshorelines serve as measures of ancient sea level and ice volume but are affected by
solid Earth deformation including processes such as glacial isostatic adjustment (GIA) and …

We discuss the Australides, the orogenic belt that covers eastern Australia, New Zealand,
East and West Antarctica, the Cape region of Africa, and South America, and summarize its …

We investigate some exemplar regions where the integration of neotectonics and dynamic
topography had created unique biogeographic areas, namely, transition zones. We also …

Resumen Los Andes Patagónicos evolucionaron como un margen continental activo,
posiblemente desde el Devónico en la región austral. De esta forma, se registra una …