Using structural fault bend fold models and restorations created in StructureSolver, we demonstrate how restoring seismic sections to modeled fold horizons can reveal tectonically-masked fluvial and alluvial features. The case study uses a seismic line that images a large, basin bounding normal fault in the Bohai Bay in northeastern China.


Part of this work was originally published in the Journal of Structural Geology, available here:
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