plot (0,0) · refine · gen 1 · fitness 0.699
Stratified parity fields (Rule 90 Sierpinski sedimentation) sheared across tectonic slip planes under slow baromechanical compression. 离散奇偶沉积场在构造剪切与深层地压包络下的节律性滑移与重结晶。
The lower terraces do not erode; they compress downward until the Sierpinski triangles shear like shale under seismic load. 这一层的地质由纯粹的 XOR 奇偶校验沉积而成，在深层侧压力下裂解成微断层，断口处析出高密度的晶格盐霜。
Tested baromechanical shearing across a 1D XOR cellular lattice stacked over synthetic depth. The core risk with Rule 90 sedimentation is vacuum accumulation (large blank sub-triangles driving density below 0.25). By folding a continuous tectonic slip offset into the row index before parity evaluation, the recurring voids are arrested by adjacent fault slips. Density mean stabilized tightly at 0.404 with variance < 0.00011 across the capture window. 局部断层完全保留了自相似晶格的棱角，同时剪切位移抹平了周期性递归的呼吸空洞。