1) listric normal fault
铲式正断层
1.
The earliest Woxi fault is a listric normal fault, formed in Xuefeng Movement(at 800 Ma or so).
沃溪断层最早形成于雪峰期 ,为铲式正断层 ;加里东期表现为右旋斜冲性质 ,西部错失鱼儿山矿体上部层脉 ,错失矿体在鱼儿山以东 ;印支—燕山期表现为左旋正滑性质。
2) Listric fault
铲式断层
1.
With the compressional stress increasing,the dip-slip motion in listric fault system could successively generate reverse-"fish-fork-shaped" structure,hanging wall interpenetration thrust,footwall shortcut thrust,"backward broken" footwall shortcut thrust imbricated fan,"backward broken interpenetration" thrust,.
随着压应力递增,铲式断层系统中的倾向滑动可渐次形成反转-"鱼叉"状构造、上盘交截冲断层、下盘捷径冲断层、"向后破裂"下盘捷径冲断层叠瓦扇、"向后破裂交截"冲断层、向前破裂后冲断层叠瓦扇、后冲断层与下盘捷径冲断层扇形构造和脊部塌陷"上突"构造等。
3) listric normal fault
铲形正断层
1.
The listric normal fault is the most universal and typical structure in the extension area.
铲形正断层是伸展构造区最普遍、最基本的断层构造。
4) listric normal faulting
铲状正断层作用
5) Listric hinge fault
铲式枢纽断层
6) istric faults
铲状断层
1.
Based on the non-similarity structure of listric faults,a configuration similarity method(CSM) is brought forward for 3D modeling of the non-similarity structure.
断层构形非相似性问题制约着三维可视化建模的发展,铲状断层表现得尤为典型。
补充资料：正断层
见断层。
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