  In this work we present a new conceptual model to describe fluid flow in a
porous media system in presence of a large fault. Geological faults are often
modeled simply as interfaces in the rock matrix, but they are complex structure
where the high strain core is surrounded by the so called damage zones,
characterized by the presence of smaller fractures which enhance the
permeability of the medium. To obtain reliable simulation outcomes these damage
zone, as well as the fault, have to be accurately described. The new model
proposed in this work considers both these two regions as lower dimensional and
embedded in the rock matrix. The model is presented, analyzed, and tested in
several configurations to prove its robustness and ability to capture many
important features, such as hight contrast and heterogeneity of permeability.
