1) dextral convergent strike slip
汇聚型右行走滑
1.
When the Cenozoic tectonic system forming, the S N tectonic system joined in it, and the S N faults were re activated by forming S N dextral convergent strike slip faults zones and transformation zones.
第三纪近南北向断裂活动以汇聚型右行走滑方式为主 ,形成近南北向走滑构造和近南北向构造变换带 ,作为深部边界约束条件而影响着第三系变形。
2) Dextral strike-slip
右行走滑
1.
Dextral strike-slip and tectonic transformation of the northern Longmen Shan fault belt from Late Neogene:A case study from the Qingchuan fault;
龙门山断裂带北段晚新近纪以来的右行走滑运动及其构造变换研究——以青川断裂为例
2.
Geodynamic mechanism of dextral strike-slip of the western-edge faults of the South China Sea
南海西缘断裂带右行走滑的地球动力学机制
3.
The ductile shear zones formed by principal deformation and metamorphism in Ningtan granite supper-units and its circumambient rocks in Nabu area of Southeastern Guangxi may be divided into two types: NE-trending dextral strike-slip ductile shear zones; NW-trending thrust-nappe ductile shear zones.
桂东南那卜地区宁潭超单元及其围岩中 ,主期变形变质作用形成的韧性剪切带可分为 2类 :NE向右行走滑性质的韧性剪切带 ;NW向逆冲推覆性质的韧性剪切带。
3) right-lateral strike-slip
右行走滑
1.
The structural planes are controlled by right-lateral strike-slip structural belt.
综合分析认为,这些结构及其分布是受右行走滑剪切带的控制。
4) dextral strike-slip thrust
右行走滑冲断
5) Thrust and dextral strike-slip
逆冲-右行走滑
补充资料：上者右行
上者右行 上者右行 运气术语。指天之气右旋。出《素问·五运行大论》。张景岳注：“上者右行，言天气右旋，自东而西以降于地。”
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