An active margin across the Adriatic Sea (central Mediterranean Sea)
New seismological and structural data from the central Adriatic—Gargano promontory area
demonstrate that the current models of an aseismic and slightly deformed Adriatic block
have to be revised. A seismically active deformational belt is mapped along two main fault
systems, the Tremiti Islands and Mattinata faults. Moreover, geologic and geophysical
evidence suggests that a more extensive lithospheric boundary may cut across the central
Italian peninsula to the Tyrrhenian basin.
demonstrate that the current models of an aseismic and slightly deformed Adriatic block
have to be revised. A seismically active deformational belt is mapped along two main fault
systems, the Tremiti Islands and Mattinata faults. Moreover, geologic and geophysical
evidence suggests that a more extensive lithospheric boundary may cut across the central
Italian peninsula to the Tyrrhenian basin.
Abstract
New seismological and structural data from the central Adriatic—Gargano promontory area demonstrate that the current models of an aseismic and slightly deformed Adriatic block have to be revised. A seismically active deformational belt is mapped along two main fault systems, the Tremiti Islands and Mattinata faults. Moreover, geologic and geophysical evidence suggests that a more extensive lithospheric boundary may cut across the central Italian peninsula to the Tyrrhenian basin.
Elsevier
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