“…In this case, rock's thermal behavior depends not only on mineralogy, but also on the proportion of each mineral in the rock, size, texture, orientation, and elastic properties as well as the anisotropy in thermal expansion of each mineral (Vázquez et al, 2011). Therefore, thermal deterioration and the way microcracks generate and grow are related to thermal diffusion, thermal expansion, mineralogy, maximum temperature attained and how quickly this is reached, as well as on, porosity, grain size and other textural factors Castro de Lima and Paraguassú, 2004;Shao et al, 1999;Vázquez et al, 2010).…”