Forward stratigraphic modeling in rift sedimentary basins

This review explores the application of Forward Stratigraphic Modeling (FSM) in rift sedimentary basins, with a special focus on the capabilities of DionisosFlow™. Rift basins, shaped by complex tectono-sedimentary processes, present modeling challenges due to their evolving accommodation space, abrupt facies transitions, and variable sediment supply. DionisosFlow™, a diffusion-based FSM software, enables 3D simulation of sedimentary architecture by integrating tectonic and thermal subsidence, sediment transport, and sea-level change. Through a comparative evaluation of case studies, including the Midyan and East African Rift basins, this review highlights how DionisosFlow™ performs in both data-rich and data-scarce frontier basins. The tool's process-based modeling framework is compared with other FSM platforms like GPM and Badlands, emphasizing their respective strengths, limitations, and application scopes. Additionally, the review addresses methodological workflows, model calibration, and the integration of geological constraints, including plume-related magmatic influences. It concludes by outlining future directions for improving FSM realism in rift settings through enhanced data integration, multi-scale modeling, and scenario testing