底缘

To widen the range of the plane gates,it is very much important for plane gates to study hemline cavitation and solving measure.

为了扩大其适用范围，对阀门底缘空化特性及改善措施进行综合研究是很有十分重要的。

Used to drive,then the pitch Circle diameter should be o less than twice of the shaft diameter.

IM3011 型为机座不带底脚，端盖有凸缘，圆锥形轴伸，轴伸向下。

The characteristics of skull bones are; underdevelopment of paramostoid process of the occipital bone; unjointing of zygomatic process from its arch with no supraorbital foramen; formation of semiglobal structure by petrous temporal bone;no naso -maxillary notch between nasal bone and nasal process of premaxilla; unobvious facial surface of lacrimal bones;well-developed nasal process of premaxilla; no facial crest of maxillae's exterior;...

头骨的主要特征是：枕骨的颈交不发达，眶上突不与颧弓相连，无眶上孔；颞骨岩部形成半球形鼓泡，鼻骨与颌前骨的鼻突之间不形成鼻颌切迹；泪骨几乎无颜面部；颌前骨的鼻突发达；上颌骨外面无面嵴；腭骨发达；犁骨腹缘后部不与鼻腔底壁接触；下颌骨支下缘无血管切迹、垂直部后下方有一角突。

The west slope of the ridge is a thrust marginal accretionary wedge.

海脊西侧缓坡为陆缘增生楔，可见刺穿现象，这些刺穿构造是由逆冲挤压引起的泥底辟。

Based on studying of these special structure bodies and fluid movement s for gas hydrate formation,six types of tectonic-controlled gas hydrate reservoirs including accretionary prism,buried anticline,basin-edge slope,fault-folded,slide and dirpir are summarized.

通过对这些特殊构造体与天然气水合物成藏关系的研究，结合流体活动对水合物形成的影响，总结出陆缘地区有增生楔型、盆缘斜坡型、埋藏背斜型、断褶型、滑塌型及底辟型等六类构造控制型水合物矿藏。

The South China Sea is located at the junction of the Eurasian, the Pacific and the Indian-Australian plates, and it is one of the complex continental margins which are of active margin in early and passive margin in late. Five tectonic types of gas hydrate deposits including accretionary prism, fault-folded, dirpir, slide type and basin-edge slope are identified in the South China Sea.

南海位于欧亚板块、太平洋板块及印澳板块的交汇处，早期为活动陆缘，晚期演化为被动陆缘，其构造活动具有早期张裂、后期挤压的特点，这既不同于被动陆缘，也有别于活动陆缘，可视为&复合型&大陆边缘，兼具了&被动陆缘沉积速率高、活动陆缘构造活跃&的优点，从而形成了&增生楔型、断褶型、底辟型、滑塌型、盆缘斜坡型&等多种构造控制型水合物矿藏，是&复合型&大陆边缘水合物成藏地质模式的典型代表。

Based on studying of these special structure bodies and fluid movements for gas hydrate formation, six types of tectonic-controlled gas hydrate reservoirs including accretionary prism, buried anticline, basin-edge slope, fault-folded, slide and dirpir are summarized.

通过对这些特殊构造体与天然气水合物成藏关系的研究，结合流体活动对水合物形成的影响，总结出陆缘地区有增生楔型、盆缘斜坡型、埋藏背斜型、断褶型、滑塌型及底辟型等六类构造控制型水合物矿藏。

Where, when brewing tea slowly sinking, due to high aroma; bitter taste of green tea, liquor color green, in the folder have aeruginous Securinega shoots; tea taste with less Shibuya thick, dark red liquor color, Securinega over Hong-Liang; whether black tea or green tea, it is thin and hard Securinega are on the folder more leaf, vein coarse, serrated leaf margin evident that this was the summer of tea.

凡冲泡时茶叶下沉较慢，香气欠高；绿茶滋味苦涩，汤色青绿，叶底中夹有铜绿色芽叶；红茶滋味欠厚带涩，汤色红暗，叶底较红亮；不论红茶还是绿茶，叶底均显得薄而较硬，对夹叶较多，叶脉较粗，叶缘锯齿明显，此为夏茶。

Based on the regional tectonic evolution, combined with the high precision isotopic ages from this paper and other geologists, we have some new acquaintances as follows: 1 There has no Caledonian granite belt distributed in north margin of North China Craton. So, the traditional evolving model of North China Carton, which formed on this idea and the acquaintance about the collision of North China plate and Siberian plate, must be incorrect; 2 The age date show that the earliest magmatic activity began since late-Palaeozoic Permian, which is inconsistent with the previous idea that there were Caledonian and Hercynian active continental margin in the north of North China Craton and in the south Xingkai Massif. 3 the crust and lithosphere were thickened by the subduction and collision of Siberia plate and North China plate during Late Paleozoic. The magma is formed when the crust is heated and melts caused by thickened lithosphere delamination and caused the Asthenosphere upwelling. But only a little basaltic magma erupted, most magma underplate under the bottom of the crust. Thermal energy derived from basaltic magma underplating made the middle and lower crust melt partially and the late Permian-early Triassic granites is formed in large scale.

根据区域构造演化分析，并结合本文及他人高精度同位素年龄，我们对延边花岗岩形成的大地构造环境有了新的认识：1在华北地台北缘并不存在所谓的加里东花岗岩带，因此，建立在此之上的传统的华北地台北缘演化模式及有关西伯利亚板块与华北板块的碰撞拼合的认识也必然是不正确的；2华北地台北缘和兴凯地块南缘不存在加里东期和海西期花岗岩带，表明两地块边缘最早的花岗质岩浆活动始于晚古生代的二叠纪，即不存在传统观点所认为的加里东期或海西期活动陆缘；3晚古生代由于西伯利亚板块与华北板块的俯冲碰撞，致使地壳和岩石圈增厚，导致加厚岩石圈发生拆沉作用，使得软流圈上涌，加热地壳使之熔融形成岩浆，但玄武质岩浆少量喷出地表，大部分底侵于地壳底部，形成下地壳高密度的玄武质底侵层，玄武质岩浆底侵的热能引起中下地壳广泛部分熔融，形成大面积分布的晚二叠世—早三叠世花岗岩。

The test results showing the variation of mid-span deflection of the heated beam against the bottom flange key temperature are given in Figure 2, together with the analytical results.

实验结果显示的受热桁条与底缘的主要温度比的中部翼展偏差值和分析结果如表2。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。