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1)  Bashan arc-shaped fault zone
巴山弧形断裂带
2)  arcuate fault
弧形断裂
1.
Based on researches on characteristics of the He125 fault,the authors have found that the arcuate fault is parallel to the fault strike and is the combination of fault-trough and fault-ridge,as evidenced from the profile.
通过对河125断层几何学特征的分析发现弧形断裂平行于断层走向剖面上表现为断槽、断脊组合;垂直于断层走向剖面上断层分为竖滑段、倾滑段和平滑段3段,生长指数规律为弧中大于弧翼,断层倾角规律为弧中小于弧翼。
2.
The arcuate fault is the combination of fault trough and fault ridge,it is found from the section that is parallel to the arcuate,the fault can be separately divided into three parts,vertical-slip part,dip-slip part and horizontal-slip part from the section that is perpendicula.
为解释断层下降盘浊积砂体横向不均一的控制机理,从河125断层几何特征入手,剖析了断层形态与浊积砂体的关系,发现弧形断裂平行于断层走向剖面上为断槽、断脊组合;在垂直于断层走向剖面上断层可分为竖滑段、倾滑段和平滑段三段。
3)  Dabashan curvilinear structural belt
大巴山弧形构造带
1.
Mesozoic deformation of Dabashan curvilinear structural belt of Qinling orogen
秦岭造山带大巴山弧形构造带中生代构造变形
4)  back range faults
后山断裂带
1.
Late Quaternary kinematic characteristic of the back range faults at the Middle Longmenshan fault zone;
龙门山中段后山断裂带晚第四纪运动特征
5)  buried-hill fractured zone
潜山断裂带
1.
Layout parameter determination in buried-hill fractured zone based on forward modeling.;
基于模型分析的潜山断裂带优化观测系统参数设计方法
6)  Shanxi rift zone
山西断裂带
1.
Analysis on horizontal deformation of Shanxi rift zone in recent years;
近几年山西断裂带水平形变的初步分析
补充资料:巴山


巴山
bashan

  巴山(b ashan)针灸穴名。出《司牧安软集》。马位于拼部,百会穴与股骨大转子连线的中点处,左右侧各一穴。皮下为拼筋膜和件浅肌,深层为拼中肌,有拼前动、静脉及份前神经分布。以火针或圆利针直祠3~4.5厘米,毫针直刺10一12厘米。主治膜胯风湿、闪伤映胯、后肢麻木。(宋大冬)
  
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