The evolution of sediment source regions in the Andes of Ecuador can be linked to Late Cretaceous-Cenozoic development of a subduction-related magmatic arc, retroarc fold-thrust belt, and flexural foreland basin. An ...

The sedimentary fill of peripheral foreland basins has the potential to preserve a record of the processes of ocean closure and continental collision (e.g., the later phases of the Wilson cycle), as well as the long-term ...

Sikinos and Ios Islands, located in the Southern Cyclades of the Aegean, are part of a Cenozoic metamorphic core complex system that exposes subduction-related rocks in the highly-extended back-arc region of the Hellenic ...