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Preliminary results of the microstructural and textural characterization of compaction bands affecting four porous carbonate formations
Processi di fagliazione nei grainstone carbonatici: implicazioni per la caratterizzazione dei serbatoi naturali di geofluidi
Permeability anisotropy of fractured and faulted tight Cretaceous platform carbonates by use of 3D fracture modelling (Agri Valley, southern Italy)
In the Agri Valley, high-angle faults crosscut platform carbonates that are analogues of the lithological units that host the deep seated largest onshore oil reservoir in Europe. The main faults are W-NW oriented with a left-lateral strike-slip kinematic; additionally, three sets of related secondary faults are present: (i) N-NE oriented with right-lateral/transtensional kinematics, (ii) E-W trending left-lateral transtensional and (iii) N-NW trending left-lateral transpressional. Two of the secondary N-NE striking faults, strike-slip and transtensional, together with the adjacent host rock, were selected to build a Discrete Fracture Network model eventually used to evaluate the hydraulic properties and permeability anisotropy of these faults. The outcomes of this modelling show that the total permeability of the fault zones is higher than that one of the host rock. Moreover, the results are consistent with the transtensional fault having higher permeability values relative to the strike-slip one. The permeability anisotropy within the fault damage zone as well as in the host rock is mainly related to the fracture orientation
Fault zone properties in the Roman Valley Quarry reservoir analogue: insights from well logs, core and field data
Structural and Time Constraints of Long-Lived, Crustal-Scale Structures in the Foreland Domains of the Apennine- Maghrebian Chain (Southern Italy): Implications for Background Deformation
A first comparison of natural and artificial shear bands in porous carbonate grainstones
Multi-scale properties of strike-slip faults corss-cutting the Pleistocene carbonate grainstones of Favignana Island (NW Sicily, Italy)
Development and distribution of bed-parallel compaction bands and pressure solution seams in carbonates (Bolognano Formation, Majella Mountain, Italy)
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