根据分形几何学的重要参数———分形维数可以反映复杂分形体空间分布的特征，将红柳地区构造层断层系作为一个平面集来进行分形维数的研究。
The fault system of structural horizon in Hongliu area was taken as a plane set to be studied with the fractal dimension.
基于构造地质学中断层、褶皱的几何形态及描述要素，总结出在地质剖面图上反映断层、褶皱的方法。
The method to show fold and fault on the section is proposed on the basis of the geometrical shape and description elements of fold and fault.
对河125断层进行了几何学再造，利用平衡剖面分析了运动学和动力学特征。
This paper analyzes the kinematics and kinetics characteristics of Fault he 125 through the analysis of balanced section and the geometric reconstruction of Fault He125.
除了深、大断裂等复杂断层以外，研究一般断层都需利用岩层、岩脉等各自的迹线。迹线的产状实质上是空间二斜面相交线的产状，属于立体几何学等数学范畴。
The respective trace of rock bed, vein must be utilized usually in the study on a fault except the complicated fault, such as deep and big fault.
除了深、大断裂等复杂断层以外，研究一般断层都需利用岩层、岩脉等各自的迹线。迹线的产状实质上是空间二斜面相交线的产状，属于立体几何学等数学范畴。
The respective trace of rock bed, vein must be utilized usually in the study on a fault except the complicated fault, such as deep and big fault.
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