Figure 3
From: Time and space scattered volcanism of Mt. Etna driven by strike-slip tectonics
Uninterpreted (a) and interpreted (b) L_01 seismic reflection line, imaging the nearshore portion of Timpe Plateau (see Fig. 1 for location). It is a tectonically raised and highly deformed sector, rooted by a high-reflective basement, pertaining to the Hyblean foreland. The plateau is characterized by a prominent push-up in its southern portion and a bland anticline in the northern one. High-reflective chaotic and blanking seismic facies point to diffuse Plio-Quaternary volcanics (orange areas) and deep magmatic intrusions (orange arrows), respectively (see text for further details).
