“… [ 8 ] ) is considered as an important model for radiation‐damaged silicates because it is able to incorporate the radioactive (U, Th) and rare‐earth impurities isomorphically and to absorb high doses of self‐irradiation by alpha particles and recoil nuclei over geological times of an order of hundreds million years. [ 2 ] The regularities of zircon radiation damage were explored using the X‐ray diffraction (XRD), [ 9,10 ] transmission electron microscopy, [ 11 ] magnetic nuclear resonance, [ 12 ] Raman and infrared (IR) spectroscopy, [ 13–15 ] measurements of the indentation hardness, [ 16 ] X‐ray photoelectron spectroscopy (XPS) [ 17 ] and computer simulation. [ 18,19 ] The crystalline‐to‐amorphous phase transformation was described in terms of two percolation transitions p1 and p2.…”