everse fault thrusts are developed at one flank of each fold in a radiating pattern in the skirt-fringe fold belt of the Taihu Dome.
即当垂直构造力向上顶托形成隆起时,岩层沿下震旦统软弱层发生垂直半径方向的收缩,产生侧向挤压,形成穹窿褶边褶皱,并在褶皱陡翼产生逆-逆冲断层,组合成放射状构造。
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