“…TD and PSD are more effective for volatiles (like H, He, Na, K, S, Ar) and have typical energy below 1 eV (dashed lines in Figure 3, left and middle refer to 2 eV Na, that is, the escape energy at Mercury), while IS and MIV are effective also for refractory species (e.g., Mg, Al, Si, and Ca), thus producing more energetic ejecta closer to stoichiometric composition. In contrast to the MIV-released particles having a Maxwellian distribution of an expected peak corresponds to ∼2500-5000 K [Eichhorn, 1978] or a peak particle energy of ∼0.6 eV, the high-energy tail of IS ejecta, SHEA, on the other hand, can in principal have surface release energies above 10 eV [Gnaser, 2007;Wiens et al, 1997], more than sufficient to escape the local gravity (e.g., 0.09 eV/nucleon for Mercury, 0.03 eV/nucleon for Moon). This means that releases from all other processes can be excluded, when analyzing IS products through SHEA detection (Figures 3, right and 2).…”