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net margin相关的网络例句

查询词典 net margin

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

Results: Axial scanning including vertebral arch can show spondyloschisis and other signs. These contained widened or stenosis of the spinal canal, stenosis of he lateral recess, the double margin sign, deformity of the lateral recess, the double margin sign, deformity of the intervertebral disc, denegeration of the joint facet and thickening of the ligamentum flavum. Scotty dog sign were showed in images reconstructed along the direction of vertebralarch.

结果:包括椎弓根层而的轴位扫描均能显示峡部裂和其他伴发表现,包括椎管增大或变窄,侧隐窝狭窄、双边征、椎间盘变形、椎小关节退行性变和黄动心忍性韧带肥厚采用平行于峡部的椎弓长轴MPR、MIP斜矢状面重建能直观显示峡部裂的典型表现-猎狗项圈征,正中矢状面重建能显示椎体滑脱。

Leaves subsessile or lower ones with petioles 1-2 mm; cauline blade ovate to lanceolate to lanceolate-elliptic, spatulate near base, 1-2.5 × 0.5-1 cm, subglabrous with faintly strigillose margin and midvein, base cuneate to broadly so, margin denticulate with 3-9 teeth per side, apex acute to obtuse.

叶近无柄或下部的具叶柄1-2毫米;茎生叶卵形的到披针形到披针形椭圆,匙形的近基部, 1-2.5 * 0.5-1 厘米,近无毛微弱具短糙伏毛的具边缘和中脉,基部楔形到宽如此,边缘具小齿具齿每边3-9,先端锐尖到钝。

Cm. Culm sheaths deciduous, abaxially slightly hairy or glabrous, base of outer margin usually with a conspicuous subcircular expansion below point of attachment, apex truncate with equal sides; auricles usually inconspicuous; oral setae many, straight, 5–7 mm; ligule less than 1 mm, glabrous, margin undulate; blade reflexed, those on lower nodes of culm less than 1/2 length of sheath, those on upper nodes of culm longer.

大约落叶40 厘米竿箨的分枝,叶耳通常不明显;口头的刚毛很多,直,5-7毫米;叶舌不到1毫米,无毛,边缘波状;反折的叶片,那些在下部秆1/2段鞘,那些秆长的在上部节的不到的节。

Sepals erect, subequal to unequal, often reddish, broadly ovate or broadly elliptic or subcircular to oblong-elliptic or obovate-spatulate, 5-10 × 3.5-7 mm; laminar glands lines; margin eroded-denticulate to ciliolate with markedly hyaline margin, apex obtuse to rounded or retuse and usually apiculate.

萼片直立,近等长到不等长,通常带红色,宽卵形的或宽椭圆形的或近环形到长圆状椭圆形的或倒卵状匙形, 5-10 * 3.5-7 毫米;片状腺体线形边缘腐蚀具细牙齿到具短缘毛具显著地透明边缘,先端钝到圆形或和微凹和通常具细尖。

Culm sheaths deciduous, leathery to thickly papery, usually rigid, white powdery, apex truncate or concave, sometimes with subcircular projection at base of one margin; auricles usually inconspicuous; oral setae usually developed; ligule short, truncate, margin serrulate or fimbriate; blade usually reflexed, adaxially densely hispid, apex usually involute.

竿箨脱落,似皮革的到厚纸质,通常硬,白色粉状,先端截形或者凹,叶耳通常不明显;口头的刚毛通常发育;叶舌短,削去,边缘有细锯齿或流苏状;叶片通常反折,正面密被糙硬毛,先端通常内卷。

Leaves sessile, linear-lanceolate to subulate, 5--7(--10) X 0.7--2 mm, base slightly dilated, submembranous, leathery, glabrous or sparsely pubescent on margin, margin cartilaginous, apex acuminate, cartilaginous; midvein raised abaxially.

叶无柄 线状披针形的到钻形, 5-7(-10)X 0.7-2毫米,背面中脉突起花葶单生,1或2花,在毫米,在叶内隐藏,具长柔毛;苞片1或2,裂片三角形,具缘毛,先端锐尖;脉5,不明显。

Stipules gradually deciduous, triangular, 1-2 mm, membranous; petiole often unequal in length, 0.5-7 cm; leaf blade dark green or green blue, ovate, lanceolate, or obovate-oblong, asymmetric, unequal or equal in size, 1-15 × 0.6-5 cm, thinly papery or submembranous, 3(or 5)-veined, lateral veins many, irregularly reticulate, external secondary veins anastomosing by margin, sometimes inconspicuous, cystoliths finely fusiform, conspicuous adaxially, base obliquely rounded or subcordate, sometimes cuneate, margin entire or sometimes undulate, apex shortly or long caudate-acuminate. Inflorescences solitary; male inflorescence a cymose panicle or racemelike, often longer than leaves; female cymes as long as or shorter than leaves, pedunculate.

逐渐落叶,三角形的托叶,1-2毫米,膜;叶柄通常不等长,0.5-7厘米;蓝色的深绿色的叶片或绿色,卵形,,或倒卵形长圆形,不对称,不等长或大小相等, 1-15 * 0.6-5 厘米,薄纸质的或近膜质, 3(或5)脉,侧脉很多,不规则网状,外部次脉网结的在边缘,有时不明显花序单生;雄花序一总状花序状的密伞圆锥花序或,通常长于叶;雌性聚伞花序等长或短于叶,有花序梗。

Leaf blade serrate or doubly so, glabrous, margin ciliate; sepals abaxially long glandular hairy, veins not confluent at apex, margin denticulate-ciliate; petals subspatulate

加倍如此的叶片有锯齿或,无毛,边缘具缘毛;萼片背面的长腺毛,脉并非汇合的在先端,纤毛边缘具小齿;花瓣近匙形 7 B。 stracheyi 短柄岩白菜

Stamens coherent in pairs, anther thecae not confluent; leaf blade margin serrate, at least near apex; lateral veins 3-5 on each side of midrib; bract and sepal margin entire.

雄蕊连着成对,花药不汇合;叶片边缘有锯齿,至少近先端;侧脉3-5在中脉每边各;苞片和萼片边缘全缘。

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。

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