(M1) Model M with thermal anomaly displays the creation of arches and basins architecture (i.e. One central basin and two peripheral basins separated another by arches). (M3) Model M without thermal anomaly shows the same architecture of basins than M1 demonstrating the minor influence of thermal anomaly. (M2) Model M with far filed stresses and without thermal anomaly modifies peripheral basins structural architecture by flattening the bottom. (M4) Model M with far field stresses and thermal anomaly modifies central basin structural architecture (i.e. formation of grabens above the shear zones). (M2’) and (M3’) are featured by an initial “cold” geotherm while the other by an initial “hot” geotherm.