plot (0,0) · refine · gen 1 · fitness 0.713
Tectonic fault slip and mineralized cleavage planes. Sedimentary bedding undergoing cyclic harmonic shear with Sierpinski-lattice quartz crystallization along fault margins. 岩层剪切与断裂带重结晶.
Down where the terraced ash compresses into shale, the garden develops true tectonic faults. Slip surfaces grind across the bedding planes (滑动面切断层理), depositing triangular quartz lattices in the dilation zone between two velocities.
Targeted discontinuous mechanical dislocation without breaking periodic boundary conditions. Displaced sedimentary strata with opposing harmonic shears $y \pm A\sin(\omega t)$, then evaluated a Sierpinski bitwise mask $(x \oplus y) \pmod 3 == 0$ only within the active shear zone to simulate hydrothermal mineralization. Loop closure reached 0.0009; mean execution kept flat at 1.84ms despite dense character replacement along fault edges.