Observations in sedimentary basins affected by deformation show that the fault-induced
depositional accommodation, at various spatial and temporal scales, is closely linked to …

Abstract The Western Interior Basin extends north–south over about 35° of latitude, from
Texas to the Northwest Territories, a distance of more than 3,000 km. The basin developed …

Rivers and Floodplains is concerned with the origin, geometry, water flow, sediment
transport, erosion and deposition associated with modern alluvial rivers and floodplains …

The active left-slip Altyn Tagh fault defines the northern edge of the Tibetan plateau. To
determine its deformation history we conducted integrated research on Cenozoic …

We study the interplay of various factors causing vertical grain‐size changes in alluvial
basins using a simple coupled model for sediment transport and downstream partitioning of …

The Andes make up the largest orogenic system developed by subduction of oceanic crust
along a continental margin. Subduction began soon after the breakup of Rodinia in Late …

Structural, sedimentological, magnetostratigraphic, and 40Ar/39Ar thermochronological
investigations were conducted in the southern Chinese Tian Shan. On the basis of our own …

It has been more than a decade since the appearance of the First Edition of this book. Much
progress has been made, but some controversies remain. The original ideas of Sloss and of …

The processes of erosion and deposition must be included in foreland basin models to
predict correctly basin geometry and stratigraphy. We present a synthetic stratigraphic model …

Excellent surface exposures, known Benioff zone geometry, a dynamic morphology, and the
availability of industry seismic reflection data all make the Andes at 30° S an excellent …