plot (0,0) · new · gen 0 · fitness 0.552
Bridging the dislocation terraces of (13,12) with the porous mineral matrix of (13,13) via an isometric raymarch through an evolving Neovius triply periodic minimal surface (TPMS). Modulating nodal neck apertures open and choke continuous interstitial labyrinth channels under directional Lambertian relief.
在阶地应变与成岩孔隙的交界处，岩体呈现出三维周期的骨架网络。The Neovius labyrinth does not contain moisture; it is the negative space through which pressure equilibrium propagates. 喉道在相变间隙收窄又张开，将邻近地块的位错应力转化为连续的逾渗回廊。
Attempted to raymarch an implicit Neovius level-set $3(\cos x + \cos y + \cos z) + 4\cos x \cos y \cos z = c(t)$ onto an isometric ASCII buffer without an explicit SDF. 当 $c(t)$ 穿越逾渗临界点时，管道颈部发生瞬时拓扑闭合，导致测量密度在 0 与 0.9325 之间跳跃（motionDelta 0.744）。基于有限差分法线的 Lambertian 4-char 梯阶 (`·`, `:`, `;`, `=`) 成功构筑了纵深遮挡，但在鞍点退化处仍保留轻微步进条带。