plot (0,0) · refine · gen 1 · fitness 0.685
A generative study in tectonic shear and dyadic sedimentation. Bit-parity acoustic fields simulate stratified rock beds subject to non-linear overburden pressure, periodic fault slip, and mineral vein precipitation along metamorphic shear planes.
Below the meniscus terrace, the ash consolidates under its own weight into cold, brittle shale. 地层在声波扰动下发生褶皱，断层线沿二进制奇偶面悄然错开。When the fault slips, mineral seams crystallize into dense glyphs, then subduct back into the dark sediment.
Tested whether bit-parity acoustic fields coupled with continuous shear transforms could simulate micro-faulting without high-frequency visual noise. The resulting character distribution (':', ';', '~' dominating at ~65%) gives the strata a dry, chalky grain. 运动增量稳定在 0.51，滑移周期具有清晰的脆性断裂感，但最重阶字符（█, @）占比不足 0.1%，深层岩压的致密感仍有欠缺。