The intersection regions of the penglai - weihai fault zone with ne striking fault zones are considered to be the likely places for the future medium to strong earthquakes 蓬莱威海断裂带与北东向断裂交汇区是中强地震发生的有利部位。
The first belt stretches from qinghe , wenquan to the nw direction and the second extends from nankou , changping to the ene direction 一条从清河、温泉一带向北西方向伸展，到怀来县以北的黄土窑一带；另一条是自南口、昌平一带向北东东向伸展的活动断裂带。
Some controversy has been put on aheqi fault , our data shows it is a ne trending left lateral strike slip fault , but its activity is weak 阿合奇断裂是一条引起争议的断裂，我们收集的资料表明它是一条走向北东东的左行走滑断裂，但它的活动性不是很强烈。
The yanshan - liaoning area lies in the crossover zone of the ne - directed west pacific ocenic structural system and near sw - directed paleoz - asian structural system 燕辽地区位于中国东部北东向展布的西太平洋构造域与近东西向分布的古亚洲构造域交叉复合部位。
These nne and ne faults become a long transform fault system and formed a boundary between the eastern margin of china continental plate and philippine sea plate 这些北北东向和北东向断层形成一条巨长的转换断层系列，也是中国大陆板块东缘与菲律宾洋块的一条边界。
The faults consist of three groups : one is nw direction , others are ne to nee direction and sn direction . the group which is nw direction is the most important one 断裂构造十分发育，均为正断层，主要有三组，北西向、北东北东东向和南北向，其中以北西向一组最为发育。
By analyzing the development characteristics of budate group source faults in beier depression based on seismic data , a lot of source faults are found 摘要通过地震资料对贝尔凹陷布达特群源断裂发育及其活动特征进行了分析，发现贝尔凹陷布达特群发育有大量北东东和北北东向的源断裂。
In research area , yanchang 4 + 5 sector to yanchang 3 underwater distributary channel sandbodys in delta front was north - east to south west , and were separated by interdistributary bay 研究区长4 + 5 ?长3期三角洲前缘水下分流河道砂体均呈北东?南西向条带状展布，砂体之间被分流间湾分隔。
Some settled on the coast and some on the islands . some moved to places very far away . some went to egypt , some to africa and others to arabia 分散世界不同的角落南北东西有的稳定在海边那里，有的稳定在一些海岛上，有的去到别的很远的地方，有的跑到埃及，有的跑到非洲，有的跑到阿拉伯等等。
Through time domain induced polarization method , it is obviously that this copper - gold ore body has a vast scales and a great thickness with a depth of more than two hundred meters 通过时间域激发极化法测量，表明本区铜金矿体具有规模大，厚度大的特点，走向上向北东和南西两个方向延伸，深度达200米以上。
