-
Analog laboratory experiments of fracture networks formed due to forced foldi...
Forced folding of a low-permeable, competent sediment layer in response to magmatic sill intrusion, remobilisation of fluidized sand or fluid overpressure in underlying porous... -
Analog laboratory experiments of gravity gliding in salt-bearing rift basins
Salt tectonic processes in rift basin are mainly driven by sub- and supra-salt faulting and sedimentary loading. However, since the formation of a rift basin is often... -
Analog laboratory experiments of the formation of forced folds and sand injec...
Sand injections form by intrusion of overpressured, fluidized sand into surrounding low-permeable, fine-grained rocks. We conducted a series of scaled analog experiments to...