1) Chennan Fault
陈南断层
1.
Tectonic positive inversion of Chennan Fault and its relation with hydrocarbon accumulation in Dongying Sag
东营凹陷陈南断层构造正反转及其油气成藏关系
2) Chenjia reverse fault
陈家逆断层
1.
Because of the separation of Chenjia reverse fault(F 1),two obviously different geological zones in structure and depositional features in Lengjia region are produced.
由于陈家逆断层 (F7)的分隔 ,冷家地区形成了东、西两套构造与沉积特征明显不同的地质区域 ,导致了两者不同的油气藏类型、分布规律和成藏条件。
3) Laoyachen Fault
老鸦陈断层
1.
In order to find out the location,characteristics and activities of the Laoyachen Fault in Zhengzhou,the high-resolution shallow seismic P and S wave survey profiling across the Laoyachen Fault was carried out at the end of 2006,and different seismic sources along with combinations of diverse observation geometries with different parameters were used.
为了查明郑州老鸦陈断层的位置、性质及其活动性,2006年底跨老鸦陈断层进行了高分辨率的浅层地震P波和S波探测,通过采用不同的地震波激发源、不同的观测系统参数相结合的工作方法,获得了沿剖面不同深度的地下细结构图像,揭示了老鸦陈断层的形态和特征。
2.
In order to find out the location, characteristics and activities of Zhengzhou Laoyachen fault, the shallow seismic surveys at different exploration depths that are across Laoyachen fault in northern area of Zhengzhou city, were carried out in 2006.
为了查明郑州老鸦陈断层的位置、性质及其活动性,2006年底,在郑州市北郊横跨老鸦陈断层进行了不同探测深度的浅层地震勘探,通过采用爆破震源和可控震源相结合、不同观测系统参数相结合的工作方法,获得了探测深度30—6000m范围内的地下结构与构造图像。
3.
Based on the research on relationship between Mangshan scarp and Laoyachen fault,and according to interpretation of remote sensing images,middle-shallow layer seismic detecting and comparison of joint drillings,measureme.
该文以邙山东侧陡坎与老鸦陈断层为例,通过遥感影像解释、中浅层地震探测、联合钻孔对比、地貌测量等方法,得到了老鸦陈断层是一条倾向NE向的前第四纪正断层,同时将陡坎分为三段,陡坎总体走向NW—NWW向,由北而南,高差逐渐降低,出郑州东南后消失。
4) fault step on steep slope
燕南断层
5) Nanling Fault
南陵断层
6) Pingnan big fault
平南大断层
1.
The relation of Pingnan big fault and hydrocarbon migration and accumulation;
平南大断层特征及与油气运聚的关系
补充资料：逆断层
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