Each segment has a distinctive difference of its own in fault geometry, associated structures, active age and the sedimentation control etc.
各分段断层的结构、形态、伴生构造、活动时间及对沉积作用的控制等都存在较明显差异。
But to the region of nappe structure, by the reason of rising reverse fault top wall, so we just can calculate the fault geometry under the footwall breakpoint.
而对于逆断层因其上盘的上升过程,使得推算的断层只能获取下盘断点以下的构造形态。
Examining the geometry of fault zones offers clues to the level and the direction of the stress exerted on the rock.
考察断层系统的几何分布可以推断出岩石所受的应力大小和方向。
Based on fractal geometry, this paper further comments on the planar distribution of faults, especially the geometric characteristics of the fault zone.
本文依据分形几何学,进一步探讨了断裂的平面分布,特别是断裂带的几何特征。
As to the method of calculating the relative movement force and total fault displacement of two walls of a fault, there are the method of descriptive geometry and the method of diagram analysis.
求解断层两盘相对运动力和总断距等的方法,美国有毕令斯的画法几何,前苏联有莫尔恰诺夫和瓦依涅尔曼的图解分析法。
The difference between these methods is in how the geometry of the fault and rupture initiations are modeled and in the statistical model used to predict the future earthquakes.
这些方法之间的区别是在怎样的几何建模和破裂,提升是错的统计模型,用来预测未来地震。
Fault development, structure geometry and reservoir lithology are the major factors to controll oil and gas distribution.
断层发育程度、构造部位、储集层岩性是控制油气分布的主要因素。
The geometry and inner structures as well as the kinematics of the east-west dextral strike-slip fault system in the middle segment of the intraplate Yanshan orogenic belt are described.
阐述了分布于燕山板内造山带中段的近东西向中生代右行走滑构造系统的几何学与运动学特征。
From structural geometry, Wuxia fault belt developed twelve structural styles, among them fault-propagation folds and buckle-propagation anticline are the most important.
从构造几何学分析来看,乌夏断裂带发育12种主要的构造样式类型,其中断层相关褶皱类型以纵弯背斜、断展背斜及其生长类型为主。
From structural geometry, Wuxia fault belt developed twelve structural styles, among them fault-propagation folds and buckle-propagation anticline are the most important.
从构造几何学分析来看,乌夏断裂带发育12种主要的构造样式类型,其中断层相关褶皱类型以纵弯背斜、断展背斜及其生长类型为主。
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