In a first lengthwise groove 6a, a second lengthwise groove 6b, and a third lengthwise groove 6c sequentially arranged in the width direction, first widthwise grooves 7a are arranged between the first and the second lengthwise grooves 6a and 6b in the length direction, and second widthwise grooves 7b are arranged between the second and the third lengthwise grooves 6b and 6c in the length direction.

相對(duì)于依次地沿所述橫向排列的第一縱向溝槽6a、第二縱向溝槽6b和第三縱向溝槽6c综合区图片区视频区亚小说区，所述第一橫向溝槽7a在所述第一和第二縱向溝槽6a国货自拍网，6b之間沿所述縱向排列，所述第二橫向溝槽7b在所述第二和第三縱向溝槽6b在线国产主播专区第一页，6c之間沿所述縱向排列国产午夜亚洲精品一级在线。

With horizontal shear component of intercolumn forces ignored, four equilibrium equations were formed, i.e., force equilibriums along the vertical direction, the sliding direction, Y axis direction, and moment equilibrium around Y axis. The equilibrium equations contained the actions of underground water, earthquake and supporting forces.

在忽略條柱間作用力的水平剪切分量的基礎(chǔ)上，建立鉛直方向久久久久久免费精品电影网、滑動(dòng)方向黄色一区二区三区无码视频网站、垂直滑動(dòng)方向的力平衡以及繞Y軸的力矩平衡共4個(gè)方程，平衡方程中納入地下水国产又粗又猛又爽的野外视频、地震www三级片网站com、支護(hù)力作用。

An accelerometer was used to record triaxial acceleration while the patient was walking (x-axis: superoinferior direction, y-axis: anteroposterior direction, and z-axis: mediolateral direction).

當(dāng)病人在步行時(shí)加速度計(jì)被用來(lái)記錄三軸的加速度（X軸亚洲欧洲美洲无码精品Va水蜜桃，上下方向aaaaaa日本，Y軸前后方向，Z軸一级花片免费直接观看，中間外側(cè)方向）。

The bodily center of gravity speed changes along the changing of the swivel posture. In the three axes of X, Y, Z, the speed is pindling and has no appearance difference in the front-to-back direction and left-to-right direction, but speed in the vertical direction is the fastest.The speed of the swinging leg appears three acceleration stages obviously.

在身體轉(zhuǎn)動(dòng)中無(wú)論手臂的引帶wwwbbbbcom、跟隨或擺動(dòng)腿的揮擺等動(dòng)作5566资源在线，正好體現(xiàn)了肢體相對(duì)身體縱軸質(zhì)量分布的改變在线一级免费在线观看，從而達(dá)到了調(diào)整身體轉(zhuǎn)動(dòng)速度的目的，所以古典芭蕾舞揮鞭腿轉(zhuǎn)720度難度動(dòng)作是滿足動(dòng)量矩守恒定律的一级e片网站。4内地三级精品自拍。

Results present that when the lateral-torsional coupling is considered, the responses in the lateral direction of the coupled system subjected to a initial disturbance and a harmonic excitation in the torsional direction, respectively, can be occurred in different forms, and show great effects. However the responses in torsional direction subjected to lateral disturbance and harmonic excitation are slightish.

對(duì)系統(tǒng)進(jìn)行了非線性響應(yīng)數(shù)值計(jì)算和相應(yīng)的頻譜分析，結(jié)果顯示彎扭耦合后白白色在线观看视频，在扭轉(zhuǎn)方向的擾動(dòng)和簡(jiǎn)諧干擾扭矩均會(huì)以不同的形式在彎曲方向表現(xiàn)出來(lái)在线黄网精品，并對(duì)系統(tǒng)的彎曲振動(dòng)產(chǎn)生較大的影響；而彎曲振動(dòng)對(duì)扭轉(zhuǎn)振動(dòng)的影響則要小得多色哟哟中文字慕。

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.

根據(jù)青藏高原東部及其鄰區(qū)布設(shè)的143個(gè)寬頻帶固定和流動(dòng)地震臺(tái)站的遠(yuǎn)震記錄的SKS波分裂分析獲得了各臺(tái)站的快波偏振方向和快慢波之間的時(shí)間延遲国产一级视频性交。

Exhibiting angle unconformities or erosion unconformities in different part of the basin, these surfaces are obvious to be recognized on seismic profiles.T1 conformity, separating Eogene from Neogene, was formed during the whole basin uplifting and erosion by the end of Eogene.T1 unconformity denuded unbearing strata differently, and the deeper and thickest erosion lies on the southern margin of the basin, which reflects the activity of southern Jiangnan paleo-terrene. In conclusion, the major erosion belts extending along NW direction reflects NE-SW compression and slipping caused the Eogene basin uplift and strengthen the earlier NW direction extending low convex, and formed the NW direction extending depress and erosion belts.

古近系和新近系之間的T1不整合面形成于古近紀(jì)末期的盆地整體抬升，對(duì)下伏地層造成不同程度的剝蝕欧美日本三级片国产馆，沿盆地南緣的剝蝕層位深日韩uuu，剝蝕量大，反映盆地南緣整體相對(duì)隆起三级插入小视频在线观看，與江南古陸的隆起作用有關(guān)国产洗澡网站。T1界面剝蝕帶走向以北西向?yàn)橹鳎从沉伺璧卦诠沤o(jì)末受到了北東－南西向的擠壓或壓扭作用自拍偷拍19页，該作用造成盆地整體抬升一个人在线视频免费观看片毛片，強(qiáng)化了北西向展布的低凸起，產(chǎn)生了近北西向的洼陷和剝蝕帶日韩精品视频网站免费观看。

To avoid this,some authors advocate the use of Herbert screws in a posterior to anterior direction,15,19,27 or the use of mini-fragment screws.1,2 Koval et al showed that the fixation strength of cancellous lag screws placed from a PA direction was stronger than that of screws placed from an AP direction.30 They hypothesized that the countersinking of the AP screws removed subchondral bone and compromised the quality of fixation.

Koval等研究表明利用網(wǎng)狀拉力鏍釘從PA位固定比AP位固定的力量要增強(qiáng)国内精品自产拍在线观看999。

In the depth scope ranging from 1100 meters to 3500 meters, the direction of the middle principal stress becomes vertical.The simulation result, from the modelling of the Kun 2# drill and its vicinities, suggests that the vertical stress variation is relatively small in the place 3 to 7 times of the drill diameter from the well wall, but the horizontal stress varies in some trend. Moreover, the direction of the minimal stress component and the remote loading pressure take place large deviation in southeast direction.

而對(duì)昆2井及其周邊地區(qū)建立了子模型進(jìn)行模擬的結(jié)果顯示，在距井壁3～7倍的地方日本sewwwcom，垂向應(yīng)力變化相對(duì)較小久久夜色精品国产欧美一，但水平應(yīng)力則發(fā)生了不同程度和趨勢(shì)的變化，另外2020国内自拍视频，最小應(yīng)力分量的方向與遠(yuǎn)源加載的壓力在南東向發(fā)生了較大的偏轉(zhuǎn)国产AV无码片毛片一级下载。

Also, the bar code line direction as far as possible and business card printing and membership card making direction is the same since business card printing and membership card-making blanket of extrusion in business card printing and membership card making direction）.

而且，條形碼的線條標(biāo)的目的給只管即便與制卡和會(huì)員卡制作標(biāo)的目的不異老女人黄色网站，因?yàn)橹瓶ê蜁?huì)員卡制作洋橡皮布的擠壓變形主給爆發(fā)在制卡和會(huì)員卡制作標(biāo)的目的上黄色网站永久。