1) Reverse strike-slip fault
逆走滑活动断裂
2) active strike slip fault
活动走滑断裂
3) Strike slipping
走滑断层活动
4) strike slip fault
走滑断裂
1.
It is suggested that there is close genetic relation between the NNE trending strike slip fault system and uranium ore formation.
通过成矿构造背景和矿床构造研究 ,本文系统论述了不同级别构造对铀成矿的控制作用 ,认为NNE向走滑断裂与铀成矿作用之间具有密切的成因联系。
2.
The intracontinental orogeny since Late Triassic time in eastern Hunan province resulted in a NNE-trending strike slip fault system,which has underwent a critical transformation of tectonic property from convergent(T3-J)to divergent(K-E1)strike slip faulting,and controlled Mesozoic-Cenozoic magmatic activities,fault basins and uranium mineralization in this region.
走滑断裂是大陆造山带中一种非常重要的构造类型，并常常成为各种流体异常活动的场所。
3.
The foliations of mylonites mostly dip steeply and a lineations are nearly horizontal, and therefore, it is a strike slip fault.
糜棱叶理产状多较陡倾，ａ线理近水平，表明为走滑断裂。
5) Strike-slip Fault
走滑断裂
1.
The tectonomagmatic belt between eastern Hunan and western Jiangxi is a significant geological anomaly area in circum-Pacific metallogenic belt, in which NNE-trending strike-slip faults directly controlled magmatism-fault basin-mineralizing process of U, W, Sn, Pb, Zn, Sb, etc.
湘赣边地区构造岩浆带是环太平洋成矿带内最重要的高值地质矿产异常区，其中ＮＮＥ向走滑断裂明显地控制了岩浆－断陷盆地和铀及钨、锡、铅、锌、锑等的成矿作用。
2.
Based on the two geological surveys of the South China Sea in 1988 and 1989,and on the analyses of a great deal of seismic reflection sections, we discern thefaults in the South-China Sea are strike-slip faults.
本文基于我所１９８８年、１９８９年两次南沙地质调查以及大量地震剖面的综合分析，系统阐述了南海西南断裂构造的特征及性质，指出南海西南主千断裂为多期活动的走滑断裂，是它们控制了油气盆地的形成与演化以及局部油气藏的形成。
3.
In the paper,the important effect and significance of strike-slip faults are discussedon the basis of researchs on coalfield structures.
本文通过对煤田构造的研究，论述了走滑断裂的重要作用及意义，文中阐明了走滑断裂的伴生构造之一──拉分盆地是重要的成油、成煤构造。
补充资料：逆走
1.退走，逃走。
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