北

Retreating, at the terminus of the Great Northern Railway, Amiens street, with constant uniform acceleration, along parallel lines meeting at infinity, if produced: along parallel lines, reproduced from infinity, with constant uniform retardation, at the terminus of the Great Northern Railway, Amiens street, returning.

637从大北铁路阿缅街终点站，不停地以标准加速度正沿着那如果延长、会在无限彼方相遇的平行线逐渐离去。沿着那重新出现在无限彼方的平行线，不断地以标准减速度，正朝着大北铁路阿缅街终点站折回来。

The structure of control earthquake is Northen Piedmont fault of Hengshan Mountain of NE strike,and the triggering seismic structure is second-order fault of NE strike.

分析了地震的发震构造，认为北东向的恒山北麓断裂是控制大同盆地的南部边界断裂，为控震构造，北西向的次级活动断层为此次地震的发震构造。

The obvious difference in the characteristics of AASW and SAMW may result in the formation of the Subantarctic Front.

在PF1以北，向北输送的南极表层水开始辐聚下沉，在下沉并北移的过程中与亚南极模态水相遇，SAMW与AASW之间温盐特征的巨大差异可能是导致亚南极锋形成的主要原因。

On the other hand, the wind stress curl anomaly also strengthens the subpolar gyre so as to cool the Kuroshio/Oyashio Extension region .

在西风应力异常持续1O年的情况下，副极地海洋涡旋异常导致的KOE区负海温异常还可以影响到北太平洋中部，因而对北太平洋中部海温的负异常起着维持的作用。

And the results indicate that the principal stress directions in study area are mainly NE-SW, and the second substage tectonic twist made the direction deflect from North to East, but the primary direction changed little; tectonic activities during the O〓～S～D stage is some violent, most of the area are under high stresses status, and rock fracture degree is correspondingly higher, as coinciding with the drill cores observation, i.

通过数值分析，模拟了塔中Ⅰ号断裂带和塔中45井三维模拟区O〓灰岩的构造应力场和应变场，结果表明：研究区主应力方向为北东～南西向，第二期的构造扭动使其由北向东发生了一定的偏转，但总的方位变化不大；O〓～S～D时期，塔中地区构造运动较强，研究区大部分处于高应力状态，岩石破裂程度较高，而岩芯观察结果也证实了这一结果，即O〓灰岩地层中早期形成的构造结构面比较发育，单个结构面的规模也较大；C～P时期，岩石的破坏程度较早期有所提高，主要表现在两个方面，一是各局部区岩石的破坏程度普遍有所提高；二是各个级别破裂区的分布范围相应地扩大了；研究区应力分布表现出明显的不均匀性，特别是剪应力，无论是O〓～S～D时期，还是C～P时期，都有很大的差异性，特别是在小断层的端部，剪应力比较集中，而且在断层的两盘，剪应力方向和大小都变化极快。

The variaition of the surface current indicates two patterns:from Novermber to next May,it is winter-time pattern,with the left months being the summer-time pattern.The pattern transformation is much slowly from the winter to the summer with～2-3 months;whereas,it is much quick from summer to winter,with only 1 month.These variabilities are mainly caused by the seasonal monsoon.

台湾海峡由南向北传的谐振潮波与由北向南来传播潮波的共同作用，K_1分潮在澎湖列岛西侧海域出现了逆时针旋转的圆流点。2006全年的观测表明，台湾海峡西侧表层流场的的变化主要为冬夏两个阶段，11-5月为冬半年，6-10月为夏半年；由冬向夏的转换较为缓慢，而由夏至冬的转换迅速，主要受制于季风。

It is also called red basin with an open syncline structure and NNE direction of fault.

秭归盆地是侏罗纪紫红色砂页岩组成的红色盆地，为一开阔的向斜构造，断裂构造为北北东向。

Due to the diverse starting and closing characters in Tunhuang North version "Mahaparinirvana Scripture" and that in the "Taisho Tripitaka", the volume division of Tunhuang North version is also examined in the chapter.

由于敦煌北本《大般涅槃经》各卷的起止与《大正藏》本不同，所以在这一章中，也对敦煌北本《大般涅槃经》的分卷情况作了考察。

When I am in the south, in the north, when she is me in the north, she is in the south......

当我在南时，她在北，当我在北时，她在南。。。。。。

The Vietcong had the full-blooded support of North Vietnam which, in turn, was backed by China and the Soviet Union.

越南南方民族解放阵线（西方人习惯称这一组织为"越共"，而我们所说的越共是北方的越南共产党）得到北越的全力支持，而北越又有中国和苏联的扶持。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。