向北

Under the guidance of the ridge east of SINLAKU, a short-term north-northwesterly track will be observed, after which both ridges will be eroded by a passing mid-latitude trough to provide room for recurvature.

森垃克东面的副高将令森垃克向西北偏北移动。预计一道西风槽将令东西两个副高减弱，所做成的空隙将会容许森垃克作出转向。

The ridge east of SINLAKU is expected to extend westward to allow a short-term north-northwesterly track, after which both ridges will be eroded by a passing mid-latitude trough to provide room for recurvature.

森垃克东面的副高将令森垃克向西北偏北移动。预计一道西风槽将於 24 至 36 小时后到来，令东西两个副高减弱，所做成的空隙将会容许森垃克作出转向。

In addition, he has been a director of the Baptist Hospital Foundations of Birmingham, the Jefferson Federal Savings and Loan Association, the Birmingham Trade Mart Authority, the Associated Industries of Alabama, and the State National Bank of North Alabama.

此外，他也未向浸会医院基础伯明翰杰弗逊的联邦储蓄和贷款协会，伯明翰集市贸易管理局，相关产业的阿拉巴马州和国国家银行北阿拉巴马。

Supracrustal sequences free of early strong deformation The early deformation of Jingangku formation complex of Hengshan Wutai group complex has formed a bedding parallel S〓 gneissic and schistosity, occasionally bedding parallel recumbent folds in layers. The early deformation of the near-horizontal ductile shearing isn't very strong in Wutai group complex. The orientation of shear movement is NNW—SSE.

经受早期强烈变形的表壳岩系岩系恒山五台岩群金岗库岩组和五台山五台岩群最早期的变形是平行地层层理的S1片麻理和片理，偶见层内的顺层掩卧褶皱，这些早期近水平韧性剪切变形在五台岩群大都不甚强烈，对地层层序的扰动也很弱，剪切运动方向是北西西——南南东向的。

During the ductile deformation, the accompanying fluid interacted intensively with the mylonite series rocks, resulting in sericitization of plagioclases, chloritization of dark minerals and cxtcnsivc carbonatization.

中文摘要：夹皮沟金矿北西向剪切带存在着长英质和镁铁质两类糜棱岩系列岩石，韧性变形中伴随的大量流体与糜棱岩之间发生了强烈的水岩反应：斜长石绢云母化和钠化。

However, the southbound side of the street has re-opened.

主道南部北向南行驶的街道已经恢复。

Combining the analysis and study on magnetic interface, the authors think that the crust structure here is controlled by "a pile up slopes poker face to face", which is a accepted as the growth model of Bohai gulf basin widely; There is a deep-major fault along northeast in west of the area. Its extension in deep is to southeastward which coincides in most of the faults in this area.

结合该地区航磁异常的分层计算与对比，认为本地区的地壳结构受渤海湾裂谷盆地的衬"倾牌组式构造"所控制，该地区西北部存在有北东向展布的深大断裂，其深部延展与本区大部分已确认的断裂深部延展方向基本一致且朝向东南。

The newly ascertained path for oil migration, which is accurately southeastward instead of coarsely southward, indicates the directions for further explorations on the compound Lukeqin block zone.

通过分析进一步确定了成藏期的油气运移方向，即鲁克沁构造带的油气运移路径和方向是由北西向南东，为鲁克沁构造带复杂断块区油气藏的进一步勘探指明了方向。

Highelevation and lowreliefsurface,which is preserved between large rivers in SE plateau,is generically linked to the lowrelief surface in plateau interior and shows a gradual transition to less preservation because of southeastwardly increased river incision.

虽然随着河流下切深度往南逐渐增加，残留面虽越来越少，但仍然可以识别，最终终止在雅砻江逆冲断裂带附近，该断裂带以南地区没有明显负地形特征。北东向展布的雅砻江逆冲断裂带对应着50～200 km宽的地形相对陡变带。

Our work shows that, because of the large-scale dextral slip along the Red River fault zone, the northwest Yunnan rift-basin region, the extensive tectonics, are formed on the end since Miocene. The extensive basins have spread southeastwardly from the Miocene to the Quaternary. Typical strike-slip deformation appears at the center segment of fault zone. The granitic body in the late-Yanshan period, the coal-basins and the drainage of Lishe River are dextrally offset in-phase. The dextral displacement since the Pliocene can be 30~32km.

研究表明：中新世以来，红河断裂带大规模右旋走滑运动在北段区主要表现为尾端拉张伸展－构成典型的滇西北裂陷盆地区，且自中新世经上新世至第四纪，伸展型盆地由西北向东南扩展；中段区为典型的右旋走滑变形区，燕山晚期花岗岩体、上新世煤盆及礼社江水系均显示为同步右旋位错。

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。