Fig. 8: Data base for lava flow mapping and fault reconstruction.
From: Pure dip-slip along the Tuz Gölü Fault Zone accommodates east-west extension of Central Anatolia
VNIR images (A, E, I), DEM curvature (2nd derivative of elevation) highlighting convex surface features such as lava flow levees, compression ridges, and fault scarp filtered to show values > 0.04 with isolated areas <25 m2 filtered out (B, F, J). Lava flow maps (including colluvium on the hanging wall, excluding erosion zones on the footwall) and piercing points on the hanging wall and footwall lobes (C, G, K). Restored (along a 60° fault plane) lava flows at the time of emplacement (inferred from ZDD ages; D, H, L). Source of DEM as in Fig. 2. Solid fault lines indicate the location of fault projected through colluvium. A dotted buried fault line indicates mass wasting or volcanic deformation of the fault, introducing additional ambiguity of fault location.
