GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 1.1 GNGTS 2023 reconstruction of the geological framework of the study area, allowed defining the seismogenic fault, not currently mapped in literature. It is a NE-SW striking (225°), high-angle (55°) fault with a left-lateral transtensional (rake -30°) kinematic, located at depth in a brittle layer of the crystalline basement confined within two regions with more ductile rheology. Reference author: Serena Panebianco - serena.panebianco@imaa.cnr.it

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