Rolando's fissure

Rolando's fissure的基本解释

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Rolando裂, 罗朗多氏裂, 罗朗多裂

与Rolando's fissure相关的网络例句 [注：此内容来源于网络，仅供参考]

There are 4 types of the pore texture for volcanic reservoir: primary vesicle—— fissure type, amygdule——fissure type, solution porosity——fissure type, and phynocryst-matrix solution porosity——fissure type.

火山岩储集的孔隙结构有4种类型，即：原生气孔——裂缝型、杏仁体内孔——裂缝型、溶蚀孔——裂缝型、斑晶溶孔——基质溶孔——裂缝型。

The thickness of the inner wall was (0.68±0.46) mm. It showed no significant difference between the two sides of the optic canal in diameters(P＞0.05).(2)The optic canal, the superior orbital fissure and the inferior orbital fissure were respectively shown as track, crack and gorge type in CT axial pictures, while in the coronal pictures, they were respectively shown as butterfly eyes, horizontal fissure and vertical fissure type.(3)The relationship of the posterior ethmoid sinus and the optic canal was: anterocanal(42.00%), semicanal(27.5%), whole-canal(18.75%),sella turcica(9.75%) and circumcanal(2.00%).(4)The relationship of the position of the sphenoidal sinus and the optic canal was:Ι degree sphenoidal sinus(20%),Π degree (63%) and Ш degree (17%).

双侧间差异均无显著性（P＞0.05）；②视神经管、眶上裂、眶下裂在CT轴位像上分别表现为&轨道状&、&裂隙状&和&狭谷状&，在冠状位像上分别表现为&蝶眼状&、水平状裂隙和垂直状裂隙；③后组筛窦与视神经管的位置关系为：管前型占42.00%、半管型占27.50%、全管型占18.75%、蝶鞍型占9.75%和管周型占2.00%；④蝶窦气化度与视神经管的位置关系为：Ι度蝶窦占20%、Π度蝶窦占63%和Ш度蝶窦占17%；⑤视神经管内侧壁骨质缺损发生率为25.5%，缺损平均长度为(5.07±2.52)mm。

The results indicate that the formation of loess vertical joints can be divided into two phases:① the formation of inner fissure, i.e. in the beginning of deposition, the undulation of terrain leads to uneven distribution of loess, then when it rains uneven collapsibility generates, which leads to generate inner fissures ;② the stage of fissure extension, namely loess continues deposition after the inner fissures have been formed, the increasing of the top pressure makes the top of inner fissure lie in the state of tensile stress, so, when the stress reaches its tensile strength, the inner fissure extends along the vertical direction and then becomes a vertical joint.

结果表明黄土垂直节理的形成可分为 2 个阶段：①内裂隙形成阶段，开始沉积时，由于地形的起伏导致黄土厚度上的分布不均匀，在降雨时产生不均匀湿陷，从而导致产生内裂隙；②裂隙扩展阶段，内裂隙形成后黄土继续堆积，顶部压力的增长致使裂隙顶部土体受到拉应力作用，当达到其抗拉强度时裂隙就会沿竖直方向产生扩张而形成垂直节理。

与Rolando's fissure相关的网络解释 [注：此内容来源于网络，仅供参考]

fissure of Rolando：中央沟

fissure 脑裂 | fissure of Rolando 中央沟 | fissure of Sylvius 外侧裂

fissure of Rolando：中心沟

fissure 脑裂 | fissure of Rolando 中心沟 | fissure of Sylvius 外侧裂

fissure of Rolando：罗朗多氏裂

fissure of nipple ==> 乳头皲裂 | fissure of Rolando ==> 罗朗多氏裂 | fissure of round ligament ==> 肝圆韧带裂