“…The endothermal peak at 580 ο C, not accompanied by any mass loss, is attributed to the transition of quartz-a to quartz-b. The high values of CO 2 loss (>600 ο C), corresponding to the decomposition of calcium carbonate, in combination to the high reverse hydraulicity index calculated in the cases where no decomposition of organic matter was noticed, further confirms the classification of the mortars as lime mortars (Table 2, Fig.5) [24]. Furthermore, the mortar aggregates are solely calcitic in the case of samples ΜΚ1, ΜΚ2,ΜΚ2b, ΜΚ4, whereas in the rest of the samples, aggregates are a mix of calcitic and silicate nature.…”