“…The variations of these properties in carbonate rocks are predominantly debated due the geometrical complexity of the pore and rock network and their susceptibility to chemical and mechanical processes at multiple scales (Anselmetti and Eberli, 1993;Eberli et al, 2003;Baechle et al, 2008;Xu and Payne, 2009;Fournier et al, 2014;Soete et al, 2015). Siliciclastic systems, on the other hand, are more homogeneous and less affected by chemical and mechanical processes.…”