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1)  contemporaneous growth faulting
同生断层活动
2)  growth fault
同生断层
1.
Based on the conclusions of source rock contrast, passage system analysis, and reservoir infilling (history), it is pointed out that, effective source rock of the upper Es~4 and middle-lower Es~3 members is connected with reservoir of the upper Es~3 member through growth faults, therefore faults play an important role in the passage system of Liangjialou oilfield.
有效烃源岩、输导体系、成藏时间及期次是成藏机理的主要研究内容,综合运用油源对比、断裂-砂体研究、油藏充注史分析结果,认为梁家楼油田下第三系沙三中+下亚段及沙四上亚段有效烃源岩主要通过同生断层与沙三上亚段储层连通,断层是输导体系的主要组成部分,断层活动产生的地震泵效应与地层流体异常高压是运移主要动力,3期断层活动史与3期油藏充注史具有良好的对应关系,成藏机理可归纳为幕式断层活动控制油气幕式运移与充注。
3)  contemporaneous fault
同生断层
1.
Quantitative study of contemporaneous fault of eastern basin oil reservoir in China;
中国东部盆地油气藏同生断层的定量研究
2.
The second-grade fault is mostly contemporaneous fault which controls desposition.
临13断块区内的断层可分为4个级序,其中二级断层多为同生断层,且对沉积的控制作用明显。
4)  syngenetic fault
同生断层
1.
The concept of syngenetic fault is known as growth fault or synsedimentary fault.
同生断层也称生长断层、同沉积断层。
5)  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。
6)  fault activity
断层活动
1.
This paper presents the quantitative analysis of fault activity intensity and regularity of Guantao formation and the systematic study of its effect on controlling the hydrocarbon accumulation.
在定量分析济阳坳陷馆陶组断层活动强度和总结断层活动规律的前提下,系统研究了该时期断层活动对油气成藏的控制。
2.
The available geological and geophysical methods fail to estimate variations of fault activity in real time intervals, such as months, years or decades.
已有的地质和地球物理方法无法对年、月、旬等现今时间尺度上的断层活动变化进行有效预测。
3.
The component,arrangement and technical indexes of the field continuous monitoring system for fault activity are intruduced.
介绍野外型断层活动连续监测系统的组成、布设及主要技术指标。
补充资料:法祥(唐同州)《净土往生传》
【法祥(唐同州)《净土往生传》】
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