“…Specifically, the samples from group A (VQ1, VQ2, VQ10, VQ12, VQ16, VQ21, VQ22, VQ32, VQ40, VQ41, and VQ46; Figure 6a and b) are characterized exclusively by pozzolan fragments, and those from group B (VQ3, VQ6, VQ7, VQ8, VQ11, VQ13, VQ14, VQ15, VQ20, VQ23, VQ24, VQ30, VQ31, VQ33, VQ34, VQ35, VQ38, and VQ39; Figure 6c and d) predominantly contain pozzolan and subordinate ceramic fragments. The mortars from group C (VQ4, VQ36, and VQ37; Figure 6e and f) contain mainly ceramic and subordinately pozzolan fragments, and the group D (VQ5 and VQ9; Figure 6g and h) samples contain the two types of fragments in similar proportions (Belfiore et al, 2014). Almost all of the examined mortars contain different types of lime-related particles, some of which partially retained the structure of the original limestone (underburned fragments; Figure 7a), while others did not (overburned fragments and relict lime clasts; Figure 7b).…”