A comparison of the geometry, spatial organization and fracture patterns associated with forced folds and buckle folds • Section 1: Numerical analysis and field study of fractures associated with compactional forced folds • Interlayer slip and joint localization in East Kaibab Monocline, Utah: filed evidence and results from numerical modelling • Differential compaction of interbedded sandstone and coal • Forced fold development within Tertiary sediments of the Alba Field, UKCS: evidence of the differential compaction and post-depositional sandstone remobilization • Section 2: Forced Folding in extensional environments • Extentional forced folding and decollement of the pre-rift series along the Rhine-graben and their influence on the geometry of the syn-rift sequences • Displacement transfer and forced folding in the Maritimes basin of Nova Scotia, eastern Canada • Late Quaternary monoclinal folding induced by caldera resurgence at Ischia • Stratal fold patterns adjacent to normal faults: observations from the Gulf of Mexico • Section 3: Forced folding in compressional and strike-slip environments • Effects of Inter-layer slip in model forced folds • Regional tectonics and fracture patterns in the Fall River Formation (Lower Cretaceous) around the Black Hills foreland uplift, western South Dakota and northeastern Wyoming • Geometry of fold arrays in the Silesian Cracovian Region of Southern Poland • Primary and ‘Forced Folds’ of the Colombia River Basalt Province, eastern Washington, USA • Section 4: Temporal and spatial relationship between forced folds and buckle folds, crustal-scale folds and fold/fracture relationships • The interplay of faulting and folding during the evolution of the Zagros deformation belt • Complex metamorphic zonation of the Thaya dome: result of buckling and gravitational collapse of an imbricated nappe sequence • Predicting patterns of strain from three-dimensional fold geometries: neutral surface folds and forced folds • Index