publicações selecionadas
- High-permeability zones in folded and faulted silicified carbonate rocks - Implications for karstified carbonate reservoirs
- Pore network characteristics as a function of diagenesis: Implications for epigenic karstification in shallow-water carbonates
- Cenozoic Fault Growth Mechanisms in the Outer Apulian Platform
- Fracture stratigraphy and DFN modelling of tight carbonates, the case study of the Lower Cretaceous carbonates exposed at the Monte Alpi (Basilicata, Italy)
- Flow pathways in multiple-direction fold hinges: Implications for fractured and karstified carbonate reservoirs
- Three-dimensional characterization of karstic dissolution zones, fracture networks, and lithostratigraphic interfaces using GPR cubes, core logs, and petrophysics: Implications for thief zones development in carbonate reservoirs
- Structural diagenesis of shallow platform carbonates: Role of early embrittlement on fracture setting and distribution, case study of Monte Alpi (Southern Apennines, Italy)
- Hydrothermal activity along a strike-slip fault zone and host units in the São Francisco Craton, Brazil - Implications for fluid flow in sedimentary basins
- Impact of fracture set scales and aperture enlargement due to karstic dissolution on the fluid flow behavior of carbonate reservoirs: A workflow to include sub-seismic fractures in 3D simulation models
- Burial stylolites enhance karst dissolution and control cave geometry in heterolithic carbonates, Salitre Formation, Brazil
- Clayey sediments analysis as a useful tool to assessing the geodynamic evolution of fold-and-thrust belts: The case study of the Monte Alpi area (southern Apennines, Italy)
- Advancements towards DFKN modelling: Incorporating fracture enlargement resulting from karstic dissolution in discrete fracture networks
- Fault-controlled upwelling of low-T hydrothermal fluids tracked by travertines in a fold-and-thrust belt, Monte Alpi, southern apennines, Italy
- Silicification, flow pathways, and deep-seated hypogene dissolution controlled by structural and stratigraphic variability in a carbonate-siliciclastic sequence (Brazil)
- Structural setting of the Monte Alpi area (Basilicata)
- Structural and sedimentary discontinuities control the generation of karst dissolution cavities in a carbonate sequence, Potiguar Basin, Brazil
- Siliciclastic content controls the sealing behavior of layers and karst development in a carbonate-siliciclastic sequence, Salitre Formation, Brazil
- Mechanical stratigraphy controls fracture pattern and karst epigenic dissolution in folded Cretaceous carbonates in semiarid Brazil