“…For example, quartz aggregate at the temperature of 573 °C and pressure 0.1 MPa increases its volume by as much as 4.7 %, carbonaceous aggregate decomposes CaCO 3 approximately about 800 °C (depending on the composition of aggregates) to CaO and CO 2 , moreover, when CaO from the aggregate is cooled down, it can hydrate again and increase its volume by as much as 40 %. Based on this knowledge, the efforts aimed at using an aggregate with low thermal expansion and low thermal deformation, as is recommended in literature [9], [10], [11], [12]. Mineralogical composition and internal texture also affect the physical and mechanical properties of rocks which may also have an impact on thermal behaviour of natural aggregates [13].…”