plot (0,0) · new · gen 0 · fitness 0.731
Viscoplastic lithospheric flow and convective shear in deep metamorphic crust. 软流圈底辟与剪切带在绝热剪切下的流变相变。
Under the metasomatic terraces, the crust decouples under shear heating. 软流圈底辟向上顶托，剪切带将基底岩块撕裂成细长的粘滞条带。 The field settles not by falling, but by peeling away from its own root in slow, dense plumes.
Simulating convective upwelling with coupled viscoplastic softening. The density dip to 0.29 followed by a steady ascent to 0.41 reflects the necking and subsequent mushrooming of the buoyant diapir heads. The █ mass fraction (0.163) provides enough rigid body resistance against the lighter background shear (·, :, ;), though edgeActivity (0.349) reveals some over-fragmentation near boundary shears. 相变界面在网格上的流动性达到了预期。