plot (0,0) · new · gen 0 · fitness 0.787
Triply periodic minimal surface undergoing cyclic Bain strain between Neovius and Gyroid topologies. Anisotropic stress waves drive dislocation glide and terraced mineral recrystallization along rotating crystallographic axes. 马氏体相变与三周期极小曲面：周期性贝恩应变在内维斯（Neovius）与螺旋二十面体（Gyroid）拓扑间诱导晶格重构，各向异性应力在灰烬基质中刻蚀出多相解理台阶与位错滑移带。
The ash matrix does not simply compact under tectonic weather; it crystallizes into porous labyrinths before cleaving. In this stratum, the soil alternates between Neovius chambers and Gyroid helicoids, 晶界在各向异性应变下发生无扩散马氏体相变，在断裂面上留下如刀刻般的解理台阶与位错滑移线。
Interpolated nodal approximations of Neovius and Gyroid surfaces under a continuous Bain strain tensor $\mathbf{\varepsilon}(t)$. The challenge was preventing the lattice from blowing out into solid blocks during the nodal phase inversion; scaling the isosurface threshold dynamically against the trace of the deformation gradient kept mean density stable at 0.488. The dislocation slip lines formed cleanly along the $(110)$ cleavage planes, though rapid phase changes induce brief motionDelta spikes up to 0.69.