“…For these dynamic methods, stratal configurations are modelled with consideration of how the system evolves through time. However, a common challenge for meandering channelized systems is the difficulty in making the models fit closely to fragmentary observations of the channel remnants, such as abandoned meanders that are evident on seismic images (Labourdette et al, 2006;Ruiu et al, 2015, Rongier et al, 2017a; the ChaRMigS method of Parquer et al, 2017; the PB-SAND method of Yan et al, 2017). A solution to this is offered by inverse (i.e., reverse) stratigraphic modelling methods (e.g., ChaRMigS method of Parquer, et al, 2017), which honour observations of abandoned meanders by integrating them into a vector-based modelling structure that can be used to determine the temporal evolution of a river channel.…”