… Direct evidence of deformation through folding and faulting of terrace landforms is
commonly absent or where present, is typically localised leading to complications in …

… Late Cenozoic environmental changes which affected European rivers are reviewed, … ,
whilst some show that fluvial activity is linked to ongoing tectonic deformation at uplift axes …

… by highly erodible late Mesozoic to Cenozoic sedimentary units, we map and correlate six
Pleistocene fluvial terraces along an ∼50 km reach of the Arkansas River valley from Canon …

… Our model, constrained by terrace stratigraphy, supports and quantifies late Cenozoic
epeirogenic uplift and warping of the Piedmont (Figure 8). Using an age of 15 ma for TL2 and …

… Most of this section addresses evidence of uplift as revealed by marine and fluvial terrace …
section); we found only evidence of soft-sediment deformation, such as may be expected in …

… on fluvial records, particularly river terrace sequences, for patterns that contribute to the
interpretation of Late Cenozoic … to slip on fault zones, or other localized deformation. One expects …

… the only Late Cenozoic deposits from any environment are Quaternary in age, often late
Quaternary. … Other values are determined using published altitudes of river terraces relative to an …

… achieved during the late Cenozoic in an area crossed by the Tejo river between the border
… four levels of terraces are distinguished. During the late Cenozoic fluvial incision stage, the …

… during the Late Cenozoic, due to the interaction between regional uplift and localised crustal
… the fluvial terrace record for evidence of analogous localised deformation along this fault. …

… of deformed fluvial terraces. Across an area exceeding 6500 km 2 that spans the Kashi
foreland in the northwestern Tarim Basin, we use these data to place temporal constraints on …