向北

By north the mass of 1000 kernel of Xiang Na seed increases, gemmiparous rate rises, mortality drops.

由北向南种子的千粒重增加、发芽率提高、死亡率下降。

It is the first time to study concealed tectonism by remote sensing、 geochemistry、geogas、radiometric Rn in Shitingjiang area. And discover WN-ES concealed fault. And form germinative lozeng fault depression in the end of left folded area of left lateral strike-slip fault.

对石亭江地区隐伏构造进行研究中，首次应用遥感、地球化学、地气法、测氡法，发现北西—南东向的走滑断层，在左行走滑断层尾部的左叠覆区形成萌芽阶段的菱形断陷。

Bobby Wester,43,a tall,goateed house-construction worker fromRocky Mount,N.C.,told of his desperate,two and a half years w-ait for a liver transplant.

博比·韦斯特，43岁，一个来自于北卡罗来纳州落基山城的高个子、长着山羊胡须的建筑工人，向人们诉说他绝望的等待了2年半的肝脏移植。

These conclusions suggest that the extrusion rate and extent to east of the material is limited, in line with the "thrust imbricated conversion - limited extrusion model."

总的来看，肃北地区的主要断裂滑动速率和逆冲速率都比较低，叠瓦状逆冲现象比较普遍，区内有断裂、盆地、褶皱等多种构造参与了变形分解和运动转化，这些结论都说明了该地区物质向东挤出的速率和幅度是有限的，符合&叠瓦状逆冲转换—有限挤出模型&。

In front of West Kunlun from south to north, the main tectonic patterns are fault and fault-related-fold, which changed from imbricated thrust to decollement structure and from basement involved to cover detachment fold.

西昆仑山前构造变形区的构造样式为断裂及其断层相关褶皱，变形顺序总体由前展式自后陆向前陆扩展，变形方式自南而北从叠瓦状逆冲向滑脱挤压过渡，从基底卷入式向盖层滑脱式过渡。

The main structure strike of Kashan area distributed in NW-SE direction.

Kashan地区的主体构造走向呈北西-南东向展布。

Along the low-angle overthrust Early Permian marble and Early Triassic sandy slate were thrust southward over Paleocene-Eocene purplish red conglomerate of the Paleocene-Eocene Fenghuoshan Group and brick-red sandy conglomerate of the Oligocene Yaxicuo Group, forming many klippen of varying scales, and thick fault brecci.

沿低角度逆冲断层，早二叠世大理岩和早三叠世砂板岩自北向南逆冲推覆于古新统—始新统风火山群紫红色砾岩和渐新世砖红色砂砾岩之上，形成大量不同规模的飞来峰；沿主逆冲断层发育厚层断层角砾岩与断层泥，局部形成碳酸盐质糜棱岩。

The granitic enclaves in the central-facies porphyroblastic lava are subvolcanic rocks with forming age of 134.2±1.9Ma. There is another intrusion of subvolcanic rhyodacitic porphyry with age of 136.0±2.6Ma, in the contact zone of the two volcanic cycles in the western part of the Xiangshan complex. The U-Pb ages of the sub-quartz-monzonite porphyry and lamprophyre are 129.5±2.0Ma and 125.1±3.1Ma, respectively. This suggests that the extension in the Xiangshan region, began in K〓, was week, and earlier than that in the coastal region of Zhejiang and Fujian provinces. Extension in K〓 in Xiangshan and neighboring regions was much stronger, forming NE striking large red-downfaulted-basins.

相山中心相碎斑熔岩中的花岗质包体属次火山岩，其成岩年龄为134.2±1.9Ma，在相山西部两火山旋回的界面之间，存在另一类次火山岩的侵位，其成岩年龄为136.0±2.6Ma，岩性为次流纹英安斑岩；次石英二长斑岩及煌斑岩的成岩年龄分别为129.5±2.0Ma及125.1±3.1Ma，说明相山地区的伸展、裂解作用明显早于浙、闽沿海，在K〓就开始了，但规模并不是很大；而K〓时期的拉张作用在相山及其邻区表现的更为强烈，形成了大面积的呈北东向展布的红色断陷盆地。

Secondary roads through this hwan Benxi, 201 National Road runs through the county from north to south, across the east-west line Lardizabalaceae.

本桓二级公路直通本溪，201国道自北向南纵贯全县，木通线横跨东西。

With the ADCPs\' profile observations,the relationship between the longshore wind and current details the northward background circulation exists all the year around from the surface to the bottom with averaged speed～10cm/s, and being 10～20cm/s in spring and summer and smaller than 5cm/s in winter.

顺岸风速与顺岸流速的统计关系以及ADCP的海流剖面观测表明，台湾海峡西侧的平均10cm/s的北向背景流常年存在，春夏季流速为10-20cm/s，冬季小于5cm/s。

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。