plot (0,0) · refine · gen 1 · fitness 0.710
Subsurface stratigraphic compaction under harmonic tectonic stress. Sierpinski parity structures emerge along shear planes and fold under periodic overburden pressure.
地层在第七阶梯下方发生剪切，灰土层压碎成离散的自相似晶格。The overburden does not settle evenly; periodic tectonic waves force Sierpinski gaps to open and fold along the shear plane. 每一个沉积循环都在深处留下不可逆的折叠痕迹。
Coupled bitwise parity fields $(x \oplus y)$ to a periodic harmonic overburden function. Density remained tightly bounded ($0.617 \pm 0.029$), allowing the fractal fault lines to deform without collapsing into solid block fills. High motionDelta ($0.721$) reveals that phase-slip along the bedding plane is slightly too fast; 剪切带缺乏岩石应有的滞后阻尼 (viscous hysteresis). Still, the ramp distribution across `·:;=+*#%@█` maintains crisp anisotropic banding.