Geofluids / 2019 / Article / Fig 2

Research Article

Structural and Mineralogical Characterization of a Fossil Hydrothermal System Located at the Outermost Front of the Southern Apennines Fold-and-Thrust Belt

Figure 2

(a) Interpreted NE-SW-oriented seismic reflection profiles 16-85 in which the main decollement and the splay thrust faults displacing the Pleistocene sedimentary succession are highlighted; (b) interpreted NE-SW-oriented seismic reflection profiles VN5 across the south-eastern sector of the study area, showing the allochthonous complex overlying the Plio-Pleistocene covers and NW-SE-directed faults displacing the Apulian Platform; (c) interpreted NW-SE-oriented seismic 18-85 across the north-western sector of the study area, showing the listric geometry of the N-S-directed fault zone that displaces gently folded Eocene-Miocene succession. See Figure 1 for location.
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