断层两盘岩层错动、错距和相对运动关系

岩层迹线是岩层在断层面上的交迹线。它和两盘相对运动力的相交关系及相对运动力在断层面上的特殊位置,可以得出岩层错动和相对运动之间三条普遍规律和三条特殊规律。六条规律普遍存在于除了具有复杂地质现象的深、大断裂等以外的一切较常见的断层中。它们之间有简易规律可循。大量立体图形显示:一般的断层都可有多种不同的力学成因;两种不同的岩错现象,也可有相同的力学成因。总错距是上下盘相当层迹线之间的最短距离,尚未被研究过。它影响到其他各种岩(地)层错距的大小及层位错动的比例。

RELATIONSHIP OF DISLOCATION, DISLOCATION DISTANCE OF TWO WALLS OF FAULT WITH RELATIVE MOVEMENT

A trace of rock bed is the interception trace of rock bed on the fault plane. According to the interception relationship of it with the relative movement force of two walls and the special position of the relative movement force on the fault plane, the 3 general rules and 3 special rules can be induced. These 6 rules are generally applicable to all usual faults except the abyssal fault with complicated geological activity. There is a simple rule between them. Many stereo-diagrams show a general fault can have many different geneses in mechanics and two different dislocations can have a same genesis in mechanics. The total dislocation distance is the shortest distance between the corresponding traces of upper and lower walls, which has not been studied yet and influenced the size of dislocation distance of other rock bed(strata) and the proportion of horizon dislocation.