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In this paper we deal with the kinematic and chronological relationships among low angle normal faults and high angle strike- to oblique-slip faults in an exhumed mineralized area, where shear veins and minor associated structures filled with the same mineral assemblage has been interpreted as indicators of coeval fault activities. The study area is located in the eastern Elba Island, where a mineralized...
Studies of fracture networks and hydrothermal mineralisation of several faults affecting Jurassic siliceous sedimentary rocks, exposed in the Rapolano geothermal area (hinterland of the Northern Apennines, Italy), allow us to characterise the fault zone architectures and their permeability features. The study structures are normal faults with displacements of anything up to 30–40m, belonging to a...
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