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向西南的

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Subject to the anticyclone anchored in central China, 21W will move along its southeastern periphery in a SW to WSW direction in the next 72 hours.

受到在中国大陆的一个反气旋影响,21W 将於未来 72 小时沿该反气旋的东南部向西南或西南偏西移动。

As for coseismic deformation of Chi-Chi earthquake, the footwall of Chelungpu Fault moved southeastwards 0.3-1.5 m, and the value was increasing toward the fault; the hanging wall moved northwestwards 1.4-7.0 m, but the value was smaller south of the Choshui River. After the Chi-Chi earthquake, the hanging wall of Chelungpu Fault was still moving west-northwestwards and kept uplifting, while the footwall gradually changed direction from ESE to WSW or even WNW, clockwise resuming to inter-seismic deformation pattern. It is interesting to notice that despite the largest coseismic deformation in the northernmost segment of Chelungpu Fault, the post-seismic deformation peaked around the epicenter of Chi-Chi earthquake.

集集地震之同震变形,在车笼埔断层下盘向东南方向位移0.30~1.5 m,且越靠近断层位移量越大;车笼埔断层上盘则向西北方向大幅位移约1.4~7.0 m,浊水溪以南的位移量较小;集集地震以后之震后变形型态,以车笼埔断层为分界,上盘在震后向西北西方向位移的型态仍与同震时相同,下盘由同震时一致性的向东南东方向,逐步向西北西或西南西方向位移,亦即在车笼埔断层下盘有逐步依顺时针方向回归至震间的滑移型态;另就位移速率而言,虽然同震变形最大地区在车笼埔断层北端,但其震后的变形量最大地区,却集中於震央位置附近;就地震循环而言,震后的6年期间仍处於地层压密重整阶段,尚未回归至该区震间阶段的位移状态。

When semidiurnal tides move from the open sea to offing, they first get the high tide in the mouth of Samen bay, then bifurcate to two branches, one goes along the northwest direction and the other goes along southwest. And it can be easily found that the moving direction of diurnal tides is obviously different from semidiurnal tides.

半日潮波,由浙江东南外海向近海传播时,首先在三门湾湾口附近达到高潮,之后又分为南北两支,一支向西北传播,另一支向西南传播,而全日潮波与半日潮波传播方向有明显的不同。

The Taipei Domain basically moved east-southeastwards or southeastwards relative to Penghu, at a rate of mm/yr from 1992 to 1998 November. The only exception is the southwest the Linkou Tableland, which moved southwestwards. Two area with larger velocities are distributed roughly sub-parallel to the river mouth of Tanshui River, while the area in between has smaller slip rate.

台北地区相对於澎湖GPS监测从1992年至1998年11月期间的位移方向,除了林口台地西南侧向西南方向位移外,其余地区大致向东南东或东南方向滑移,其地表水平位移速率大多在5 mm/yr以下,出现位移速率较大的两个区块连线与淡水河出海口的方向平行,另两个区块中间则呈现位移速率较小的情形。

CP9 (X = 501 860, Y = 705 035); thence in a southwesterly direction to Corner Point No.

Eailroad Area的东北边的两个区域:第一个区域:从隅角点CP7(X = 501 810,Y == 705 010)起,边界线向东北方向延伸至隅角点CP8(X = 501 840,Y = 705 050);从该点起向东南方向延伸至隅角点CP9(X = 501 860,Y = 705 035);从该点起向西南方向延伸至隅角点CP10(X = 501 785, Y = 704 935)。

There are Hannan block in the northwest and Huangling block in the east. Its extended direction is east-northeast in the northwest area, east-west in the middle area and east-northeast in the southeast area,being a southwestward arc made up of many thrust nappes.

该带西北端受汉南地块限制,东部有黄陵地块的阻挡,其展布方向由西北部的北北东向、中部的近东西向、至东南部的北东东向,呈一向西南凸出的弧形,是由一系列呈向西南突出的巨型逆冲推覆断裂带构成。

Fortunately, the desertification degree decreased obviously, and moderate and light desertification took the leading position. From 1986 to 2003, the spatial centroid of desertification landscape patches expanded southwestward and northeastward, giving serious threat to the ecological safety of the southeast and northeast loess gully and hilly areas.

沙漠化程度明显下降,沙漠化主导类型已由严重沙漠化转变为中度和轻度沙漠化。1986-2003年沙漠化景观整体上向西南和东北方向扩展,严重威胁着西南和东北部黄土丘陵区的生态安全。

Researchers from several universities in the United States also say the February 27th quake was so powerful it moved the capital of Santiago about 27 centimeters to the west-southwest.

美国几所大学的研究人员还说,2月27日发生的地震强度之大,导致智利首都圣地亚哥也向西南西方向移位大约27厘米。

HMS Renown was clawing her way southward under reefed topsails, a westerly wind laying her over as she thrashed along, heading for those latitudes where she would pick up the northeast trade wind and be able to run direct to her destination in the West Indies.

收了上桅,名望号向西南方向慢慢滑行着。她在西风吹拂下逆浪而行,开往东北季风带,之后她就能直接驶向西印度的目的地了。风呼啸着穿过紧绷的绳索,在布什的耳边咆哮着。

This period of the Ming Great Wall, about 363 kilometers east from the Gansu-Qinghai border village at the turn Ledu County aloe flower Wan beginning, through the ditch to the northwest extension of the ice, and mutual aid county Songhua top phase; from the southwest along the reach mutual Sakamoto Mountain Risk, and the western slope of the Great Wall in Datong County phase; across the West through the empress Mountain Chase Insurance and Huangzhong County-phase; Huangzhong County, Linkou from the incense start arc from north to south ridge of mountains extending to pull together constitute the arch of the Xining Defense system.

这段长约363千米的明长城东端从甘青接壤处的乐都县芦花乡转花湾村始,经冰沟向西北延伸,与互助县松花顶相接;从互助向西南沿达坂山山险与大通县西坡长城相接;横贯大通向西通过娘娘山山险与湟中县相接;湟中县从香林口开始,南北向弧形延伸至拉脊山,共同对西宁构成拱形防御体系。

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