Rheological behaviour along the Hellenic Subduction Zone and the Adria-Eurasia continental collision

Based on the approach and workflow of the recently proposed 3D thermo-rheological model of the broader Aegean Region (Maggini et al., 2023), the present work focuses on the rheological properties corresponding to both the slab interface of the Hellenic Subduction Zone (HSZ) and the basal thrust of the Adriatic-Eurasian Continental Collision Zone (CCZ). For the purpose of this note, the geometry of the interfaces (Figure 1) was mainly reconstructed on the basis of the results of Bocchini et al. (2018), especially for the HSZ sector, and Halpaap et al. (2018) for the continental collision zone. For the Montenegro sector of the CCZ, the results of Schmitz et al. (2020) were also considered.