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英語人>詞典>漢英 : 近中切的 的英文翻譯,例句
近中切的 的英文翻譯www,国产AV,com、例句

近中切的

基本解釋 (translations)
mesioincisal

更多網(wǎng)絡(luò)例句與近中切的相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來源于網(wǎng)絡(luò)性爱免费网,僅供參考]

For the compressible materials, in order to satisfy the higher-order compatibility equation of the rate of deformation in the centered fan sector, which is a quite difficult problem unresolved in the previous studies, a particular term must be added to the expansions of the stress components in the regular logarithmic power series adopted by many researchers before. A higher-order near tip field with tangential velocity jump ahead of the crack tip is derived first, of which the dominant terms are the solution widely accepted.

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The detailed comparisons between the higher—order near tip solution and the well—known modified Prandtl field are also given in this paper.For the compressible materials, in order to satisfy the higher-order compatibility equation of the rate of deformation in the centered fan sector, which is a quite difficult problem unresolved in the previous studies, a particular term must be added to the expansions of the stress components in the regular logarithmic power series adopted by many researchers before. A higher-order near tip field with tangential velocity jump ahead of the crack tip is derived first, of which the dominant terms are the solution widely accepted.

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The evolution process under the control of the multigeodynamic force system (including the boundary forces of Eurasia-Pacific-Indian three massive plates around Nansha block, effects of the deep mantle, relative soft layer-sliding planes within Nansha lithosphere block and the earth's rotational inertial force) can be briefly divided four stages: the late Cretaceous to the early Eocene stage of uprilfing-erosion and shear-extension caused by the oceanwards-eastwards withdrew of Pacific subduction zone and the delamination of proto-subducted slab after the stage of pre-Cretaceous pre-rifting active continentoceanic plate margin. In this stage, the Nansha transcrustal layering-block started to move southeastwards on the Nansha transcrustal layer-sliding plane, meanwhile, the Andu-Bisheng and Liyue-Banyue basement layering-block slid on their upper-crust layer-sliding planes, and Xibu accretion zone was formed. Successively, it entered the stage of the mid-Eocene to early Oligocene, when NW-SE sea-floor spreading occurred in the southwest subbasin owing to the slip-line field initiated by the collision between the Indian and Eurasian plates, Zengmu foreland-basin started to develop in the same time. And in the stage of late Oligocene to early Miocene, near NS simple-shear extension and sea-floor spreading in the central subbasin of eastern South China Sea resulted from the south-southeastwards drawing-force of the mantle-flow. The crustal layering-blocks and the Miri accretion zone formed also in this stage.

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Upper and lower incisor both had controlled tipping movement. The crown of incisor moved mesially and had root apex were fixed relatively. The center of rotation was close to root apex. The upper and lower molar moved differently.

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The position changes of mandibular molars were measured from mesiodistal direction and vertical direction, and the implant anchorage loss was evaluated by maxillary central incisor.

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Finite strain measures and kinematic vorticity analysis of deformed granite in mylonitic zone show that ductile shear zone is between plane strain and constraint strain and belongs to lengthening-thinning shear zone. Sub-striking stretch lineation in ductile shear zone and dip strea on brittle fault surface are not result of transferring of lineation but production of different deformations.

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However, relating to investigate the modes, courses and characteristics of the orogenetic process in Paleozoic and after orogenetic process, the cognitive divergence have still occurred.

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Study shows that the E-W-trending steep foliation belt is one of the major structural patterns, which is well-preserved in the complex. The large-scaled ETSFB is characterized by well-developed E-W-trending steep-dipping foliations and sub-vertical folds, suggesting pure shearing under the condition of crust contraction.

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cut out:切出

由于骨量丟失和骨結(jié)構(gòu)不良,對螺釘把持力下降,傳統(tǒng)鎖釘可發(fā)生"切出"(cut out)而致內(nèi)固定失敗. 在治療老年股骨近端骨折時,髓內(nèi)固定裝置中的髖拉力螺釘(lag screw)更易出現(xiàn)這種情況. 而FixionTM系統(tǒng)采用自鎖方式,

hummocky cross-bedding:丘狀交錯層理

層系中的細(xì)層亦可大致平行層系洼狀交錯層理 洼狀交錯層理(swaley cross bedding)是彼此以低角度交切的淺洼坑,淺洼坑的寬度一般為1~5米,其內(nèi)充填的細(xì)層與淺坑底界面平行,而向上變成很緩的波狀并近于平行的丘狀交錯層理 丘狀交錯層理(hummocky cross bedding)由一些大的寬緩波狀層系組成,

Megachile:切葉蜂屬

膜翅目(Hymenoptera)切葉蜂科(Megachilidae)昆蟲,尤指切葉蜂屬(Megachile)昆蟲. 與其他近緣的蜂類相異處為,前者將花粉收集於腹部,後者將花粉收集於後足. 雌蜂獨居,與雄蜂交配後在土中A级毛片18以上观看免费网站、空植物桿或樹洞內(nèi)作巢,用綠葉碎片襯墊以包住所產(chǎn)的卵.

Megachilidae:切葉蜂科

膜翅目(Hymenoptera)切葉蜂科(Megachilidae)昆蟲,尤指切葉蜂屬(Megachile)昆蟲. 與其他近緣的蜂類相異處為,前者將花粉收集於腹部,後者將花粉收集於後足. 雌蜂獨居,與雄蜂交配後在土中、空植物桿或樹洞內(nèi)作巢,用綠葉碎片襯墊以包住所產(chǎn)的卵.

cingula:帶, 扣帶

39. fulcrum 支點成年免费人人操、軸 | 40. cingula 帶, 扣帶 | 41. mesio-incisal 近中切的