This dextral shear movement began at about 220 Ma.
松潘—甘孜板块的构造介入,可能是右行剪切作用形成的直接原因。
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
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。
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。
