Lattice Boltzmann Simulations of Fluid Flow in Continental Carbonate Reservoir Rocks and in Upscaled Rock Models Generated with Multiple-Point Geostatistics

<div>Dominant lithofacies types in the studied continental carbonate quarries. (a) Subhorizontal facies with pseudofenestral porosity (arrows). (b) Cascade facies with dendrite crusts (arrow 1) and shelter pores (arrow 2). (c) Reed facies with reed moldic porosity (arrows). (d) Waterfall facies with plant framework porosity (arrows).</div>

Geofluids

fig1

Figure 1

Figure 1: Lattice Boltzmann Simulations of Fluid Flow in Continental Carbonate Reservoir Rocks and in Upscaled Rock Models Generated with Multiple-Point Geostatistics 

Figure 1 | Lattice Boltzmann Simulations of Fluid Flow in Continental Carbonate Reservoir Rocks and in Upscaled Rock Models Generated with Multiple-Point Geostatistics 