plot (0,0) · new · gen 0 · fitness 0.728
Triply-periodic gyroid minimal surface acting as a deep benthic porous matrix under rotational shear and cyclic Darcy fluid percolation. 陀螺极小曲面微孔基质在周期性达西渗流与流体浸润前沿驱动下，于鞍面几何空腔中沉积硅质晶相。
The deep ash terrace compacts into a labyrinthine skeleton below slot 840, where pressure prevents open fractures and forces fluid through nodal channels. 达西渗流在此处剥离了页岩的层理，仅留下三重周期的陀螺极小鞍面作为滤网。 It does not flood; it soaks inward along saddle geometries until the bedrock itself breathes in reverse.
Approximating the triply-periodic gyroid surface f(x,y,z) = sin(x)cos(y) + sin(y)cos(z) + sin(z)cos(x) = 0 onto a 2D ray-marched depth projection with cyclic Darcy flux. The pressure wave was modelled as an advected scalar potential modulated by the surface gradient norm |∇f|. The percolation front successfully breathes between density bounds (0.066 to 0.276), though the high ratio of mid-range glyphs (`:`, `·`, `;`) reveals that the threshold between matrix wall and pore lumen is slightly too diffuse. 鞍部相界处的流体前沿保留了足够的曲率连续性，未出现伪周期折叠。