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clockwise rotation相关的网络例句

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与 clockwise rotation 相关的网络例句 [注:此内容来源于网络,仅供参考]

Look closely, you can tell the girls in the image above clockwise or counter-clockwise rotating rotation?

仔细观察,你能说出上图中的女孩是在顺时针旋转还是逆时针旋转?

The research results imply that the regional tectonic stress field has resulted in deformation and flow of upper mantle material with clockwise rotation,and make the alignment of upper mantle peridotite lattice parallel to the direction of material deformation. The deformation of the crust and upper mantle is possibly vertically coherent deformation.

研究表明青藏高原东北缘上地幔物质在区域构造应力场的作用下,发生了顺时针旋转的形变以至流动,使得上地幔中橄榄岩的晶格排列方向平行于物质形变或流动方向,上地幔变形和上覆地壳变形可能存在垂直连贯变形特征。

Combined the geological analysis with analogue modeling experiments,the evolution of the Yinggehai basin could be divided into four main stages:(1) Before 42Ma,controlled by the southeastward extension of the Beibu Gulf basin on the northern continental margin,the Yinggehai basin experienced dextral pull-apart.Bounded by NS-trending Yingxi fault,the transtensional areas mainly are the northwest part and along the eastern boundary of the basin.(2) From 42 to 21Ma,the development of the main rift body in Yinggehai basin was mainly controlled by the southward slip and clockwise rotation of the Indochina block along the Red River fault zone,and the sedimentation was strengthened due to the sinistral transtension.In the east,the subsidence is deepened due to the dextral transtension.(3) From 21 to 10.4Ma,the sinistral movement of the Indochina block slowed down to still.From 21 to 15.5Ma,the northwest part of the basin began to inverse locally because of post-rift thermal subsidence of the whole basin.(4) From 10.4Ma to present,the basin was affected by the dextral movement of the South China block along the Red River fault zone and thermal accident in a new phase at 5Ma.

结合地质分析和物理模拟实验,莺歌海盆地的演化大致可以分为以下4个主要阶段:早期(42 Ma以前)主要受到南海北部陆缘裂解造成的右旋转换伸展作用的影响,但影响范围较小,主要为莺歌海盆地西北部和东部边界。42~21 Ma期间,主要受控于印支地块左行走滑和顺时针旋转作用的影响,莺歌海盆地在此期间发育了主体裂陷体系,东侧受到右旋转换伸展应力场的叠加影响而导致沉降加强;21~10.4 Ma期间,受印支地块逐渐减弱直至停止的左行走滑作用的影响,盆地西北部在21~15.5 Ma期间发生局部反转褶皱,但盆地整体进入以热沉降为主的时期;10.4 Ma以后,盆地受华南地块沿红河断裂右旋走滑作用和5 Ma以后新一期热事件的影响。

As a consequence of this angle variation, the upper side of the car moves in the same sense of the forcing action (as a matter of fact , the negative values of _ indicate a clockwise rotation of the car, observed from the front side).

作为这角度变异结果,汽车的上部移动强迫的行动的同一感觉(实际上, _的消极价值表明汽车的顺时针方向旋转,观察从前方)。

The Go moved backward with 1.35mm and upward with 1.90mm in group I, the gonial angle increased for 3.69°, and angle between palatal plane and mandibular plane was increased for 5.00°; In group II, the Go moved backward with 1.85mm and upward with 3.32mm , the gonial angle increased for 4.06°, and angle between palatal plane and mandibular plane was increased for 5.22°. Both in group I and II, there was a tread for clockwise rotation of mandibular corpus. The length of pterygomasseteric sling was mild increased due to the backward movement of Go.

在Go点的变动方面,在Me点向前位移的族群里,术后Go点平均向后1.35mm,向上1.90mm, gonial angle 平均增大3.69度,腭平面与下颚平面的夹角则是增加5.00度;在Me点向后位移的族群里,术后Go点平均向后1.85mm,向上3.32mm, gonial angle 平均增大4.06度,腭平面与下颚平面的夹角则是增加5.22度,不论是向前或是向后的族群,结果皆显示翼咀嚼肌悬吊带有轻微被拉长的迹象。

Based on the SKSwave splitting analysis on the seismic records at 143 broadband permanent and temporary stations deployed in the eastern Tibetan Plateau and its vicinity, we have determined the fast polarization direction and delay time between fast and slow waves at individual stations; the pattern of SKSsplitting fast polarization direction exhibits the flow direction of upper mantles material in the eastern Tibetan Plateau, i.e., the clockwise rotation around the Eastern Himalayan Syntaxis.

根据青藏高原东部及其邻区布设的143个宽频带固定和流动地震台站的远震记录的SKS波分裂分析获得了各台站的快波偏振方向和快慢波之间的时间延迟。

There was a good correlation between Ptw,AVCtw,MVOtw,PTV,PUV,UntwR and age.2.Assessment of left ventricular twisting and untwisting of DCM patients19 DCM patients(range 18-80 yr,mean age 50.52±17.52 yr,2 females) and 21 age- and sex-matched normal controls(range18-80 yr,mean age 49.05±16.94 yr,5 females) were enrolled into this study.Then DCM patients were divided into two groups:E/A<2 group and E/A>2 group.The routine echo showed the left ventricle dilated and EF decreased.The results show that LV rotation degree, rotation velocity at baseline and apex were irregular changeable with the cardiac cycle;the rotation direction was clockwise at the base and counterclockwise at the apex,and are combined to yield a systolic counterclockwise twisting as seen from the apex,but the rotation at the basal and apex were the same direction in some patients.

扩心病患者左室扭转及解旋特征的研究选择扩张型心肌病(Dilated Cardiomyopathy,DCM)组患者19例(男性17例,女性2例,年龄18~82岁,平均50.52±17.52岁),健康体检者21例(男性16例,女性5例,年龄18~80岁,平均49.05±16.94岁)作为对照组,扩心病患者按照E/A分为E/A<2、E/A>2两个亚组,结果显示:常规超声显示DCM组LVDd值增大,EF值减小;DCM患者左室心底部与心尖部心肌旋转角度、旋转速度随心动周期变化曲线明显紊乱;与正常组比较,DCM患者左室整体扭转角度和速度分别为(6.49±1.82)°、(67.84±15.60)°/s,较正常人显著减低P<0.01左室舒张末及收缩末扭转角度DCM患者较正常人显著减低(P<0.01,左室舒张末及收缩末时间在DCM-E/A>2组较正常人及DCM-E/A<2组显著缩短P<0.01DCM患者左室解旋速度较正常人亦显著减低(P<0.01,左室功能轻中度减低(DCM-E/A<2)患者解旋率[(0.29±0.07)%]较正常人[(0.42±0.11)%]明显减低,但当左室功能重度减低(DCM-E/A>2)时左室解旋率[(0.63±0.35)%]较正常人反而增加;左室整体扭转角度、舒张末扭转角度、收缩末扭转角度、解旋与左室射血分数未见明显相关性。3。

This chassis is along anti-clockwise rotation at the same time, above three small swivel chairs also in revolving!

这个底盘是顺逆时针转动的同时,上面三个小转椅也在旋转哦!

2 Release the lock nut, according to anti-clockwise rotation, adjustment screw until the air so far excluded from the safety valve.

4.1.2 松开锁定螺母,按逆时针方向旋转,调节螺杆,直至从安全阀排除空气为止。

Firstly, saltating sand grains in various height layers mostly rotate clockwise; the rate of counterclockwise rotation changes from 16.7 to 33.3% for three different friction wind speed (u*= 0.67, 0.83, and 0.87 m/s). However, their mean rotational speeds were not significantly different, irrespective of whether the grains rotated clockwise or counterclockwise. The mean counterclockwise rotational speeds of sand grains for friction wind speed u*= 0.67, 0.83, and 0.87 m/s were 427, 519, and 604 rev/s, versus 429, 522, and 609 rev/s, respectively, in the clockwise direction.

首先,风沙流中各高度层内跃移沙粒旋转均以顺时针方向为主,逆时针方向旋转的沙粒数仅占总数的16.7-29.5%,但是无论逆时针还是顺时针旋转的沙粒,它们的平均旋转速度几乎没有差别(如u*=0.67 m/s时,分别为427 rev/s和429 rev/s;u*=0.83 m/s,分别为519 rev/s和522 rev/s;u*=0.87 m/s,分别为604 rev/s和609 rev/s);不同摩阻风速条件下各高度层内沙粒的旋转速度均服从Lorentzian分布。

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