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对瑞士赫尔文特推复体的灰岩中的共轭雁行脉列进行了研究。它们可被分成两大类:原生的和叠加的。对其几何形态的研究表明,小脉是同构造的,充填张裂而成的,它是由剪切带运动而派生的次级应力场所引起的。小脉与脉列的夹角一般变化在20°到45°左右,与作用在剪切带上的正应力大小有关。共轭雁行脉列的形成反映了岩石处于脆性到韧性的过渡的变形状态,与一定的形成深度有关。不同世代的脉反映了推复体形成和置位过程中的不同阶段。
Conjugated geese in the limestone of the Helvette, Switzerland, were studied. They can be divided into two main categories: native and superposed. The study of its geometry shows that the veins are isomorphic and filled with cracks. It is caused by the secondary stress field derived from the shear band movement. The angle between the veins and the pulse train generally varies from about 20 ° to about 45 °, which is related to the magnitude of the normal stress acting on the shear zone. The formation of conjugate geesetride pulse train reflects the deformation state of the rock in the transition from brittleness to ductility, which is related to the formation depth. The different generations of veins reflect the different stages of the formation and placement of the restoration.