We investigate the permeability and flow effects of deformation bands in porous granular carbonate rocks in Malta and use results from flow simulations to discuss the practical implications of deformation bands in carbonate and siliciclastic reservoirs rocks in general. Image- and laboratory-based analyses of deformation bands show permeabilities that are 1 – 2 orders of magnitude lower than the adjacent host rocks. Small-scale outcrop-based flow models (1 × 1 m) focus on the effect of deformation band on flow at the scale of individual bands. Two-phase flow simulations (water displacing oil) show that at the local scale a decrease in deformation band permeability led to increasing flow complexity, reduced and irregular waterfront propagati...
The gross environment of deposition has been recognised as a major influence on the development of d...
Deformation bands are strain localisation features common in highly porous clastic sedimentary bodie...
Deformation bands are strain localisation features common in highly porous clastic sedimentary bodie...
We investigate the permeability and flow effects of deformation bands in porous granular carbonate r...
Deformation bands are tabular, sub- centimeter thick zones, which accommodates shear and/or volumetr...
Many siliciclastic reservoirs contain millimetre-scale diagenetic and structural phenomena affecting...
Deformation bands are the primary structural element of fault damage zones within porous granular ro...
Deformation bands are the primary structural element of fault damage zones within porous granular ro...
Small scale deformation structures that mostly occur in highly porous rocks are called deformation b...
Deformation bands are common structures in deformed porous rocks and sediments, that localise strain...
Deformation bands are common structures in deformed porous rocks and sediments, that localise strain...
Accurate determination of petrophysical and multiphase flow properties in sandstones is necessary fo...
Accurate determination of petrophysical and multiphase flow properties in sandstones is necessary fo...
Accurate determination of petrophysical and multiphase flow properties in sandstones is necessary fo...
Deformation bands in porous sandstones have been extensively studied for four decades, whereas compa...
The gross environment of deposition has been recognised as a major influence on the development of d...
Deformation bands are strain localisation features common in highly porous clastic sedimentary bodie...
Deformation bands are strain localisation features common in highly porous clastic sedimentary bodie...
We investigate the permeability and flow effects of deformation bands in porous granular carbonate r...
Deformation bands are tabular, sub- centimeter thick zones, which accommodates shear and/or volumetr...
Many siliciclastic reservoirs contain millimetre-scale diagenetic and structural phenomena affecting...
Deformation bands are the primary structural element of fault damage zones within porous granular ro...
Deformation bands are the primary structural element of fault damage zones within porous granular ro...
Small scale deformation structures that mostly occur in highly porous rocks are called deformation b...
Deformation bands are common structures in deformed porous rocks and sediments, that localise strain...
Deformation bands are common structures in deformed porous rocks and sediments, that localise strain...
Accurate determination of petrophysical and multiphase flow properties in sandstones is necessary fo...
Accurate determination of petrophysical and multiphase flow properties in sandstones is necessary fo...
Accurate determination of petrophysical and multiphase flow properties in sandstones is necessary fo...
Deformation bands in porous sandstones have been extensively studied for four decades, whereas compa...
The gross environment of deposition has been recognised as a major influence on the development of d...
Deformation bands are strain localisation features common in highly porous clastic sedimentary bodie...
Deformation bands are strain localisation features common in highly porous clastic sedimentary bodie...