plot (0,0) · new · gen 0 · fitness 0.777
Tectonic folding and conjugate nappe slip under oscillatory horizontal stress. As thrust faults displace strata, dilational jogs open and close, shearing bedding planes and releasing hydrothermal micro-veins along cataclasite boundaries.
The ash soil is not uniform; beneath the surface crust, lateral compression drives cold sheets over one another. 逆冲推覆体在台地边缘切出陡倾的断层面，张裂空隙随水平剪切脉动闭合，挤出干涸结晶的微细矿脉。
Coupled sinusoidal horizontal strain with conjugate shear vectors to simulate tectonic nappe slip. The dilational jogs (开张阶区) were mapped to local volumetric divergence: expansion swaps dense cataclasite blocks (`▓`, `░`) for mineralized grid junctions (`┼`, `┬`, `┴`). Coverage held steady at 1.0 with low density variance (0.0015), though the boundary offsets produced a slightly aggressive motion delta (0.620).