“…As we may see for instance in Fig. 9a and b the Clapeyron slopes between tridymite and cristobalite polymorphs are well reproduced within the limits of reversal experiments [87,88,91,92]. It should be stressed that, in the case of phase transition with a wide Tref-Tλ gap and a marked Clapeyron slope (such as for the case of cristobalite, outlined in Fig.…”