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Subjects complained of unusual discharge and 20.0% complained of irregular vaginal bleeding while 34.0% with no symptoms. 4.0% patients cervix appeared grossly normal and 96% presented cervical erosion of various extents, with or without postcoital bleeding. 30.0% cases revealed abnormal cells among the 10 patients who took the Pap smear examination while the proportion is 90.0% among the 30 patients who took TCT procedure.

其中48例平均初次性生活年龄21.9岁,46.0%的患者主诉白带异常,20.0%主诉阴道不规则流血,34.0%患者无明显不适主诉。4.0%患者妇科检查未见异常,其余96%患者表现为不同程度宫颈糜烂,伴或不伴接触性出血。10例患者行巴氏涂片,仅30.0%提示异常,30例患者行新柏氏液基薄层细胞学检查,90.0%发现异常细胞。

Swallow Stone color more yellow-green, occasionally purple-brown, is a thin calcareous shale or marl.

燕子石色多黄绿,间或紫褐色,属薄层钙质泥岩或泥灰岩。

Coronal sect ional images of a series of 0.2 man-thick cryosecfions of wrist joint specimens were obtained.

方法]获取腕关节0.2mm厚的薄层冠状断层标本,在计算机上对腕骨及主要韧带的断层图像轮廓进行数据分割、对位重建和三维显示。

ConclusionThe different pole range of thin-layer chromatograms of Oviductus Ranae is set up.

结论建立了不同极性范围内的哈蟆油薄层色谱图。

Result: In the same chromatogram and on the same place of control herb, subject herb appeared well-separated spot, but no spots in negative control herb .

结果: 在同一薄层色谱中,和药材对照品相同的位置上,供试品显清晰分离良好的斑点,阴性对照品无此斑点。

The clearance after crystal is muddy: The clearance after crystal is the cavity of one layer optics after crystal center is straight, the forehead that funnel state vitreous body is in charge of is in the center of, namely the forehead of primitive vitreous body.

晶体后间隙混浊:晶体后间隙为晶体中心直后的一薄层光学空腔,中央为漏斗状玻璃体管的前部,即原始玻璃体的前部。

Moving load ; Mach number ; ground vibration ; finite element method ; thin layer element

移动荷载;马赫数;地基振动;有限元方法;薄层单元

Melting point 3410 ℃, boiling point 560 ℃, relative density of 1935, F the external electronic structure of 5d46s2, in the chemical reaction time is very easy to lose 1-6 electronic, but also can get 1-2 electronic, so oxidation number of 0,± 1,± 2, 3, 4 , 5 and 6, with 6 price of the most stable compounds, such as WO3 does not dissolve in water, the air will form in the tungsten trioxide thin protective layer of tungsten, tungsten with fluorine at room temperature, chemical combination, red hot when there is no moisture and Bromine iodide together, red hot when you can and water reaction WO3, at room temperature reaction of tungsten with aqua regia, but the hot concentrated hydrochloric acid and sulfuric acid can only be played with its weak response, but molten nitrate, nitrite, too Hydrogen peroxide, sulfur steam, steam and other phosphorus can play intense reaction, high temperature can not be carbon, boron and silicon reaction of binary compounds, widely used in industrial tungsten steel and tungsten carbide, pure tungsten filament is used to the system, and X-ray tube Tube heating components, semiconductor components can be prepared tungsten silicide, tungsten industrial production is white or black tungsten ore tungsten ore refining.

熔点3410℃,沸点560℃,相对密度1935,F外围电子结构为5d46s2,在化学反应时很容易丢掉1—6个电子,也能得到1—2个电子,所以氧化数为0、±1、±2、+3、+4、+5和+6,以+6价化合物最稳定,如WO3不溶于水,空气中的钨会形成薄层三氧化钨保护层,钨能与氟在室温下化合,红热并无潮气时能与溴、碘化合,红热时还能和水反应生成WO3,室温下钨可与王水反应,但热的浓盐酸和硫酸只能与其起微弱反应,但对熔融的硝酸盐、亚硝酸盐、过氧化氢、硫蒸汽、磷蒸汽等能起激烈反应,高温下不能与碳、硼和硅反应生成二元化合物,工业上广泛使用钨钢和碳化钨,纯钨用来制灯丝、电子管和X射线管的发热元件,硅化钨可制半导体元件,钨工业生产是将白钨矿石或黑钨矿石精炼。

P72 Formation process of roddings: B type lineation is formed by the fold rolling of the thin-bedded vein quartzite or quartzite intercalated in the rocks.

Q 0 10cm 2。杆状构造形成过程:B型线理,由岩层中夹薄层脉石英或石英经褶皱的辗滚作用而形成。

Predepositional ichnocoenosis mainly occurred in thin-bedded fine sandstone, siltstone and silty mudstone, belonging to shallow lacustrine deposits under normal climate condition.

沉积前遗迹群落主要产在属于正常天气下浅湖相薄层状粉、细砂岩和粉砂质泥岩沉积中。

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Finally, according to market conditions and market products this article paper analyzes the trends in the development of camera technology, and designs a color night vision camera.

最后根据市场情况和市面上产品的情况分析了摄像机技术的发展趋势,并设计了一款彩色夜视摄像机。

Only person height weeds and the fierce looks stone idles were there.

只有半人深的荒草和龇牙咧嘴的神像。

This dramatic range, steeper than the Himalayas, is the upturned rim of the eastern edge of Tibet, a plateau that has risen to 5 km in response to the slow but un stoppable collision of India with Asia that began about 55 million years ago and which continues unabated today.

这一引人注目的地域范围,比喜马拉雅山更加陡峭,是处于西藏东部边缘的朝上翻的边框地带。响应启始于约5500万年前的、缓慢的但却不可阻挡的印度与亚洲地壳板块碰撞,高原已上升至五千米,这种碰撞持续至今,毫无衰退。