ΔΩ ΔΩ is a multi-channel metric for measuring structural deformation in regime geography. By separating agreement drift, support erosion, and boundary displacement, Recursion Geometry distinguishes numerical degradation from true model collapse.
Regime Geography as a First-Class Object Recursion Geometry formalizes regime geography as a first-class object: a deterministic mapping from parameter space to dynamical class. Through versioned atlases and three-channel ΔΩ diagnostics, we shift from trajectory analysis to cartographic science.