1) fault activity rate
断层活动速率
1.
This paper,starting with the activity differences between the major and secondary faults in different tectonic settings,uses the fault activity rate (FAR) method to analyze and summarize the relationship between fault activities and hydrocarbon migration & accumulation during the Neotectonic period and to reveal the mechanism of late hydrocarbon accumulation in the study area.
利用断层活动速率的方法,从主次断层活动性在不同构造部位的差异方面入手,分析并总结郯庐断裂带渤中-渤南段新构造运动期断层活动性与油气运聚保存的关系,揭示在强烈活动构造背景下晚期油气成藏机理。
2.
According to the development features of the strata in Nanyang Sag,the activity history of the boundary fault are analyzed by means of fault activity rate.
针对南阳凹陷地层发育的特点,运用断层活动速率的方法分析边界断层的活动历史,认为断层活动在时间上经历了最弱—增强—最强的变化,在空间上活动强度最大的部位发生了迁移,同一时期不同部位活动强度差异明显,并结合沉积相的展布初步探讨了断层活动对沉积的控制作用。
2) fault activity velocity
断层活动速率
1.
Analysis on the fault activity velocity(Vf) shows that the oil source faults has sustaining and successive characterization,and there were two larger activity periods in Tertiary:one occurred in the later Es3 period,the other occurred in Es,or Ed period.
断层活动速率分析表明,油源断层在古近纪—新近纪表现为持续性和继承性的活动规律,呈现出2个高峰期,即沙三段上亚段沉积时期的一次大规模活动及沙一段和东营组沉积时期的另一次较大规模活动。
2.
Based on calculation of fault activity velocity, the activities of the nearly EW-trending faults in the Hefei basin were analyzed.
利用断层活动速率法定量分析了合肥盆地主要近东西向断层的活动规律,并分析了它们形成与演化的控制因素。
3) fault activity ratios
断裂活动速率
4) fault slip rate
断层滑动速率
1.
Some views from the analyses of sequence stratigraphic architecture and the relevant experiments results of Zscape model are:(1) there are an inverse relationship between the fan area and the fault slip rate;(2) the progra.
Zscape模型的相关实验结果与层序地层结构的分析认为:(1)扇面积与断层滑动速率成反比;(2)高水位期大量沉积物进积是断层滑动速率减小所引发的;(3)层序界面的形成与低水位和水进沉积是降水速率变化所致。
5) Fault motion rate
断层运动速率
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：X线断层照片
X线断层照片
参见"X线 体层摄影"。
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