Fig. 9
From: Volcanism in slab tear faults is larger than in island-arcs and back-arcs
2.5D magnetic forward models of the Enotrio volcano. Comparison between the recovered model and the observed magnetic anomaly assuming a distribution of high magnetized lava flows (5.5 A/m) confined within a layer B (blue continuous line in the bottom panel) and a distribution of the modeled magnetic anomaly profile with a distribution of high magnetized volcanic products (5.5 A/m) constrained between the bathymetry and an gently sloping plane (layer A, black broken line). The bedrock is supposed a continental crust with low magnetization (0.8 A/m)
