Disaggregation of probabilistic seismic hazard allows to quantify how much one or more earthquake scenarios contribute to the occurrence [exceedance] of a ground motion intensity measure false(IMfalse)$( {IM} )$ threshold of interest (x) at the construction site. The scenario is usually defined in terms of magnitude (M), source‐to‐site distance (R), and possibly includes the standardized residual (ε) of the ground motion model considered in the hazard analysis. Analytically, in case occurrence is of interest, disaggregation provides the joint probability density function of false{M,Rfalse}$\{ {M,R} \}$ or false{M,R,εfalse}$\{ {M,R,\varepsilon } \}$ conditional on the IM=x$IM = x$ event, that is, fM,R|IM=x${f}_{M,R|IM = x}$ or fM,R,ε|IM=x${f}_{M,R,\varepsilon |IM = x}$. Occurrence disaggregation is important for a number of earthquake engineering applications, and it is typically addressed in the literature in an approximated manner, considering as the conditioning event IM∈false(x,x+Δxfalse)$IM \in ( {x,x + \Delta x} )$, with normalΔx$\Delta x$ being an arbitrary finite width of the interval. This short communication undertakes a deeper examination of occurrence disaggregation clarifying that: (i) no approximation is needed in the case of disaggregation in terms of magnitude and distance (i.e., when fM,R|IM=x${f}_{M,R|IM = x}$ is sought); (ii) fM,R,ε|IM=x${f}_{M,R,\varepsilon |IM = x}$ is theoretically degenerate, and as such, its approximation via finite normalΔx$\Delta x$ can lead to misleading results; (iii) if normalΔx$\Delta x$ is chosen coherently with the discretization of the false{M,R,εfalse}$\{ {M,R,\varepsilon } \}$ domain used in the hazard integral, it leads to approximated fM,R|IM=x${f}_{M,R|IM = x}$, enabling the conclusion that false{M,R,εfalse}$\{ {M,R,\varepsilon } \}$ occurrence disaggregation does not add information with respect to false{M,Rfalse}$\{ {M,R} \}$ disaggregation.