Thrust in the Lurestan region of the Zagros

3D model of an growth wedge in Middle jurassic limestones, carried on top of a rigth-dipping thrust. The wedge corresponds to leftward thinning Middle Jurassic strata (having on top quaternary talus deposits), overlying right-dipping Early Jurassic dolostones. The dolostones are in turn in the hanging wal of a right-dipping thrust, whihc has a footwall syncline cored by Middle Jurassic limestone. Additional details can be fond in this scientific paper, in figure 12: https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018TC005192