“…Both effects are caused by the development of small vertical compaction strains (ε < 1%) in the reservoir as the effective stress increases during reduction of the pore pressure, typically by several tens of MPa (Morton et al, 2001;Mallman & Zoback, 2007). Reservoir compaction is generally assumed to be poroelastic (Bourne et al, 2014;Dempsey & Suckale, 2017;Zbinden et al, 2017), hence reversible, rate insensitive, and easily quantified (Wang, 2000). However, both field data (Santarelli et al, 1998) and experimental studies have shown that, even at the small reservoirs strains pertaining to hydrocarbon production, a significant part of the deformation behavior of sandstone reservoirs is inelastic (Bernabe et al, 1994;Schutjens et al, 1995;Hol et al, 2015Hol et al, , 2018Yale & Swami, 2017;Pijnenburg et al, 2018Pijnenburg et al, , 2019.…”