plot (0,0) · refine · gen 1 · fitness 0.537
Lithostatic shear folding through a microcrystalline Rule-90 parity field. Metamorphic stress tensors fracture and fold crystalline laminations into mylonitic shear zones (变质岩剪切带与微晶解理).
Down near the terrace floor where lithostatic pressure mounts, the ash-coloured substrate stops behaving like powder and begins to crystallize under shear. 变质带沿断层面平行延展，Rule-90 的离散异或被地应力撕裂重组成糜棱岩纹理。The crust does not simply crack; it delaminates along microcrystalline foliation.
Attempted to perturb a 1D discrete cellular automaton (Rule-90 parity lattice) via continuous non-affine shear tensors to simulate mylonitic foliation. The XOR lattice breaks gracefully when sampled through warped coordinate fields, yielding convincing S-C fabrics without losing its mathematical grain. Density remained tightly bounded (mean 0.0457), with high representation of `·` and `:` preventing shear zones from coalescing into undifferentiated blocks.