1) differential fault
差动断层
2) fault throw
断层落差
1.
The parameters of Quaternary fault activities such as the growth index,fault throw and fault activity rate are calculated to analyze the characteristics of fault activities in the Huimin subbasin and four orders of subbasin-controlling faults are distinguished.
通过计算断层活动性参数(生长指数、断层落差和断层活动速率),优选断层活动速率参数,分析了凹陷内断裂活动的特征,划分出四级控凹断层。
2.
Some conclusions drawn from the fault throw analysis of Zhen①、Zhen②' and Zhen② faults,are as follows:Zhen① fault forms in Taizhou period and acts intensively in Funing period.
强烈的构造运动使高邮凹陷南部断阶带主控断层上升盘遭受剥蚀而缺失大套地层,难以用常规方法对其进行研究,而断层落差分析法恰恰能弥补这一不足,从而可以明确断层形成时期及发育历史。
3) fault fall
断层落差
1.
The laws of fault activities in Zhanhua sag were studied by fault fall method.
应用断层落差法对沾化凹陷断层活动规律进行了研究。
2.
Growth fault fall is defined as the layer thickness difference between two walls, and paleo fall of certain moment is defined as the sedimentary thickness difference of this moment, which can be measured and calculated directly by structural evolvement section or geologic section and top and bottom contour maps.
生长断层落差可以根据对构造演化剖面或地质剖面的直接测量而计算 ,也可以对经时深转换的地震剖面进行测量而计算 ,还能够通过某地层顶、底构造图的深度计算。
4) fault throw method
断层落差法
1.
The characteristics of the fault activities in Shahejie-Dongying period in Huiming Sag are researched by fault throw method.
应用断层落差法,对惠民凹陷沙河街—东营期的断裂活动特征进行了研究。
2.
The characteristics of the fault activities of Shahejie-Dongying periods were researched by the fault throw method in Dongying depression.
应用断层落差法对东营凹陷沙河街—东营期的断裂活动特征进行了研究。
5) splintered fault scarp
参差断层崖
6) fault movement
断层活动
1.
For studying the coorelation between the crustal deformation and fault movement caused by the reservoir impoundment the tilt data of two fixed deformation stations(Zhouping and Yichang) are analysed and processed with wavelet transformation method.
为研究三峡水库蓄水所引起的库区地壳形变和断层活动,运用小波变换分析和处理了大坝附近两个定点形变台(周坪台和宜昌台)的倾斜观测数据,发现蓄水后库区仙女山断裂带的活动发生了一些变化,库区周围的倾斜场发生微动态变化,库区下游区域的倾斜场没有发生明显的变化。
2.
As regards the fault movement,in the west,the faults are predominantly normal and in the east the thrust faults are the most.
华北地区 (特别是西部 )的断层活动主要具有正断性质 ,但华北东部的逆断活动比例高于西部。
3.
The deformation fields raised by fault movement and a general inverse algorithm are discussed.
讨论了断层活动引起的变形场及一般性反演方法。
补充资料：落差
1.因河床高度的变化所产生的水位差数。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条