“…1,2 A wide variety of compounds with different types of bonding such as covalent ͑SiO 2 ͒, ionic ͑LiKSO 4 ͒, molecular ͑SnI 4 ͒, and hydrogen bonding ͑H 2 O͒ have exhibited the phenomenon. [3][4][5][6] In addition, systems with more complex bonding such as those in silicates, 7 tungstates, 8 molybdates, 9 and other minerals 10 are also found to undergo amorphization at high pressure. A number of factors such as metastable melting, 6 kinetic hindrance of phase transition, 11 dynamical instability, 12 polytetrahedral packing, 13 and orientational disorder of polyatomic ions 14 have been argued to be responsible for this.…”