向北

We went up North and made a beachhead in North Korea and on to a place called the Chosin Reservoir.

我们向北航行，在北朝鲜登陆，一直向北行军，到了一个叫做长津水库的地方。

The project site is bound by North Claiborne Street to the south and extends north to Bayou Bienvenue.

项目向南延展到北Claiborne大街向北延展到Bienvenue河口。

The UHPM belt Overlie the north Dabie metamorphic complex to the north and underlie the Susong metamorphic complex.

超高压变质岩向北覆于北大别变质杂岩之上，向南伏于宿松变质杂岩之下。

The evolution process under the control of the multigeodynamic force system (including the boundary forces of Eurasia-Pacific-Indian three massive plates around Nansha block, effects of the deep mantle, relative soft layer-sliding planes within Nansha lithosphere block and the earth's rotational inertial force) can be briefly divided four stages: the late Cretaceous to the early Eocene stage of uprilfing-erosion and shear-extension caused by the oceanwards-eastwards withdrew of Pacific subduction zone and the delamination of proto-subducted slab after the stage of pre-Cretaceous pre-rifting active continentoceanic plate margin. In this stage, the Nansha transcrustal layering-block started to move southeastwards on the Nansha transcrustal layer-sliding plane, meanwhile, the Andu-Bisheng and Liyue-Banyue basement layering-block slid on their upper-crust layer-sliding planes, and Xibu accretion zone was formed. Successively, it entered the stage of the mid-Eocene to early Oligocene, when NW-SE sea-floor spreading occurred in the southwest subbasin owing to the slip-line field initiated by the collision between the Indian and Eurasian plates, Zengmu foreland-basin started to develop in the same time. And in the stage of late Oligocene to early Miocene, near NS simple-shear extension and sea-floor spreading in the central subbasin of eastern South China Sea resulted from the south-southeastwards drawing-force of the mantle-flow. The crustal layering-blocks and the Miri accretion zone formed also in this stage.

南沙岩石圈新生代微板块及板内层块构造的动力演化过程，在多元动力等因素(如块体之外的欧-太-印三大板块运动边界力和地幔深部活动因素、块体内部软弱层滑面以及地球自转变化)控制下，大致经历了4个阶段的演化：从前晚白垩世的裂前活动陆-洋板块边缘阶段因太平洋俯冲带向东跃迁、原向NNW俯冲消亡的板片的拆沉、幔隆而进入晚白垩世-早始新世的隆升剥蚀、剪切伸展演化阶段，南沙超壳层块顺超壳层滑面祥东南运移、安渡-毕生与礼乐-半月基底层块沿上壳层滑面拆离，西布增生带形成；继而先后在中始新世-早渐新世期间受印-欧板块碰撞滑线场、地球自转加速影响出现西南海盆NW-SE向海底扩张和曾母前陆盆地的发育，和晚渐新世-早中新世期间南—东南向地幔流牵引造成的中央次海盆近NS向单剪伸展与海底扩张、壳体层块向南差异滑移、米里增生带形成；中中新世以来，印度-澳洲板块快速向北俯冲，构成今日南海格局。

An ancient Roman road in Italy built by Gaius Flaminius in 220 BC; extends north from Rome to Cisalpine Gaul.

一条在公元前年建在意大利佛兰明尼亚圣加伊乌斯的罗马大路；从罗马向北一直延伸至阿尔卑斯山南侧的高卢；北票自助建站版权申明：本站北票自助建站文章均来自网络。

The high Mg^# calc-alkaline and high Mg^# shoshonitic series in Qiangtang-Mangkang area indicate some intracontinental subduction happened ever in the middle part of the plateau, then the subducted slab broke off and asthenosphere was upwelled 30Ma ago, while the lithospheric mantle was melt to form low Mg^# peralkaline potassic, ultrapotassic series.

综合地球物理资料，提出青藏高原在印度大陆岩石圈的强力楔入下，高原内部软流圈物质沿欧亚岩石圈地幔俯冲板片的顶部向北东和南东挤出，使上覆岩石圈地幔发生剪切破裂，形成一系列串珠状高速体与低速体的相间分布，并随时间不断向北扩展。

In Songliao basin, the stronge tectonic inversion occurred in the Late Mingshui Formation, and during the declining of compressive force from the SSE to the NNW, the reactivation of basement faults formed positive inversion faults; released from thermal fluid diapirs, CO2 was migrated upward and then accumulated in inversion structural belts; as the development of fault-style inversion tectonics in the southern part is better than the northern part, and the western is better than the eastern part, CO2 is richer in the south than in the north, richer in the west than in the east in Songliao basin.

松辽盆地强烈的构造反转发生在明水组末期，挤压应力自南南东向北北西方向衰减的过程中，基底断裂复活形成正反转断层，CO2气从热流底辟体中脱出上运而聚集在反转构造带上，断层式反转构造南部比北部发育，西部比东部发育，因此松辽盆地南部比北部、西部比东部CO2气更富集。

Since mid-Miocene, the sea floor spreading stopped and the southwardsubduction of north-wall blocks in the southern boundary zone ofNansha transcrustal layering-block stopped and turned to north-northwestwards thrust of the south-wall blocks.

此时，南海海底扩张停止，南沙南缘的向南俯冲停止而转为南盘岩块的向北—北西逆冲推覆。

This sinistral faulting resulted from high-speed NNW-oblique subduction of the Izanagi plate in the Pacific region, and represents the typical Peri-Pacific tectonic regime and the turning point of the tectonic framework in East China.

这次左行平移是太平洋区伊泽纳崎板块向北北西向高速斜向俯冲的结果，属于典型的滨太平洋构造，可能代表了中国东部构造格局转换的开始。

The Izanagi sub-plate, the most active one of paleo-Pacific plate, subduction into east Asian with NW orientation during Jurassic, resulted in the NW compression and shortening of continental China and its adjacent areas in a whole, most areas of south China then suffered from contraction, inducing a series of small-scale intermountain basins; whereas for the eastern segment of Nanling, including most areas of western Fujian, southern Jiangxi and northern Guangdong, the stress was of extensional regime, resulted in the formation of rifting basins.

进入侏罗纪以来，作用最强的古太平洋板块中的伊佐奈歧板块朝北西方向运移、俯冲到东亚大陆之下，使中国大陆及邻区受到较强的总体上向北西的挤压和缩短作用，华南大部分地区处于挤压环境，形成一系列小型山间盆地；而在南岭东段闽西、赣南、粤北一带产生拉张背景，形成裂谷盆地。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。