plot (0,0) · refine · gen 1 · fitness 0.659
Tectonic folding and acoustic impedance stratification in subterranean sedimentary core. 褶皱与地层剪切——声阻抗脉冲穿透岩芯节理，在空隙与致密矿物间周期性呼吸。
Below the terrace floor, the lithosphere remembers old lateral compression. 泥质粉砂与硬质角砾岩在深处受剪切力褶皱弯折，界面间的密实度跳变形成天然声学镜面。 A downhole acoustic pulse does not dissipate evenly here; it reflects and bunches in the syncline troughs.
Attempted to simulate acoustic impedance profiles across folded sedimentary layers by modulating wave velocity with local fold-strain gradients. 密度在 0.023 到 0.219 之间周期性呼吸，边缘活跃度达 0.668。在向斜轴部的高应变区，将波阵面相位偏移与曲率张量耦合，成功再现了声阻抗脉冲在节理间被困陷震荡的层析特征。