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

Miocene strike‐slip tectonics was responsible for creating and closing short‐lived (ca. 6 Ma)
passages and the emergence of isolated topography in the Northern Andes. These …

The collision of intra-oceanic arcs with continental margins is a primary factor controlling the
evolution, modification, and growth of continental crust. Syn-to post-collisional basins are …

The Cretaceous units exposed in the northwestern segment of the Colombian Andes
preserve the record of extensional and compressional tectonics prior to the collision with …

Isotopic and geochemical data delineate passive margin, rift and active margin cycles in
northwestern South America since~ 623 Ma, spanning from the Iapetus Wilson Cycle …

The Cretaceous tectonic evolution of the western margin of South America involves a shift
from an extensional convergent margin toward a more compressional setting that marks the …

Monogenetic volcanic fields are commonly related to rifts and/or intraplate tectonic settings.
However, they are also less commonly recognised in subduction zones, including both front …

Abstract Between the Late Cretaceous and Paleogene, the Northern Andes experienced
subduction and collision due to the convergence between the oceanic Caribbean Plate and …

The onset of deformation in the northern Andes is overprinted by subsequent stages of basin
deformation, complicating the examination of competing models illustrating potential …

Field, petrographic, and geochemical characterization along with U-Pb zircon
geochronology of the Jurassic plutons exposed in the Upper Magdalena Valley (Colombia) …