The critical temperature range of FSCs was 400–600 °C.
The relationship between compressive strength and UPV was Weibull distribution.
An exponential relationship between splitting tensile strength and UPV was observed.
Compared to unheated FSC, the porosity value was more than trebled after exposure to 1000 °C.
Svyatoslavite that was a new crystalline phase was observed at 1000 °C.