“…In case of the Noyant stone, the weathering by crystallizing gypsum was mainly restricted to the microporous matrix of the stone, while in case of the Lede stone, several foraminifera and shell fragments were preferentially recrystallized. In general, the underlying microstructure determines the weathering pattern of the stone.Different techniques have been used to characterize natural building stones and their weathering patterns ranging from optical inspection and optical microscopy (Bai et al, 2003;Kapsalas et al, 2007) to SEM, infrared and X-ray diffraction (Maravelaki-Kalaitzaki and Biscontin, 1999;Montana et al, 2008;Thomachot-Schneider et al, 2008;Thomachot and Jeannette, 2004). Recently, new techniques like high resolution X-ray computed tomography (HRXCT) are being addressed in the assessments of weathering of natural building materials (Bugani et al, 2008;Cnudde et al, 2004;De Graef et al, 2005;De Muynck et al, 2011;Rozenbaum, 2011).…”