“…Experimental and modelling results usually show enhanced fracture closure rates at high closure stress and temperature, low Young's modulus and high amount of soft minerals, low fraction of proppants with small size, low fracture roughness and minor shear displacement (minor self-propping). The presence of water also accelerates the rate of fracture permeability reduction, in particular for clay-rich shales (Akrad et al, 2011;Alramahi and Sundberg, 2012;Guo and Liu, 2012;Kassis and Sondergeld, 2010;LaFollette and Carman, 2010;Liu and Sharma, 2005;Morales p [4] et Pedlow and Sharma, 2014;Reinicke et al, 2010;Stegent et al, 2010;Volk et al, 1981;Zhang et al, 2013;Zhang et al, 2015;Zhang et al, 2016b). The brittleness of shales, which correlates to some extent with their composition and elastic properties (Rybacki et al, 2016;Zhang et al, 2016a), may be also relevant for the long-term fracture healing rate.…”