Evidence of multifractal nature of target-evaporated slow particles produced in ultrarelativistic heavy ion interactions

Abstract

The multifractal nature of target residues in ${}^{16}\mathrm{O}\ensuremath{-}\mathrm{A}\mathrm{g}\mathrm{B}\mathrm{r}$ interactions at $60A\mathrm{GeV}$ and ${}^{32}\mathrm{S}\ensuremath{-}\mathrm{A}\mathrm{g}\mathrm{B}\mathrm{r}$ interactions at $200A\mathrm{GeV}$ has been observed using the $〈{G}_{q}〉$-moment and T-moment (Takagi's) methods.