1) Fault motion rate
断层运动速率
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 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。
4) 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。
5) fault movement
断层运动
1.
A physical model for describing the fault movement along plate boundary is proposed, i.
提出了一种描述板块边界断层运动的力学模型，即将板块边界的地壳运动表述为板块的相对刚体运动加边界断层面上的负位错分布。
2.
In addition, the potential function of the process of fault movement is set up.
建立了断层运动过程中的势函数，在此基础上，通过对平衡曲面方程的Ｔａｙｌｏｒ级数展开，求取了其标准形式，结合Ｔｈｏｍ的Ａ３类尖点突变，讨论了在不同情况下断层的活动方式。
6) Average slipping rate of fault
断层平均滑动速率
补充资料：南美洲运动会和南十字运动会
1922年在巴西举行过1届南美洲运动会,参加者限于南美洲国家。1978年在玻利维亚举行过 1届南十字运动会，参加国有阿根廷、玻利维亚、巴西、智利、厄瓜多尔、巴拉圭、秘鲁和乌拉圭8国。
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