相似形構造 的英文怎麼說

中文拼音 [xiāngxínggòuzào]
相似形構造 英文
similar-type structure
  • : 相Ⅰ名詞1 (相貌; 外貌) looks; appearance 2 (坐、立等的姿態) bearing; posture 3 [物理學] (相位...
  • : Ⅰ動詞1 (構造; 組合) construct; form; compose 2 (結成) fabricate; make up 3 (建造; 架屋) bui...
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • 相似 : 1. (相像) resemble; be similar; be alike 2. (相像處; 類似物) similarity; similitude; analogue
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  1. Conscious that the human organism, normally capable of sustaining an atmospheric pressure of 19 tons, when elevated to a considerable altitude in the terrestrial atmosphere suffered with arithmetical progression of intensity, according as the line of demarcation between troposphere and stratosphere was approximated, from nasal hemorrhage, impeded respiration and vertigo, when proposing this problem for solution he had conjectured as a working hypothesis which could not be proved impossible that a more adaptable and differently anatomically constructed race of beings might subsist otherwise under martian, mercurial, veneral, jovian, saturnian, neptunian or uranian sufficient and equivalent conditions, though an apogean humanity of beings created in varying forms with finite differences resulting similar to the whole and to one another would probably there as here remain inalterably and inalienably attached to vanities, to vanities of vanities and all that is vanity

    人體組織通常能夠抗得住十九噸的氣壓169 ,可是一旦在地球的大氣層里上升到當的高度,越是接近對流層與平流層的境界線,鼻孔出血吸呼困難以及眩暈,隨著算術級數就越發嚴重起來。他曉得這一點,尋求解答時就設想出這樣一個難以證明是不可能的行之有效的假定:倘若換個更富於適應性,解剖學上的也有所不同的種族,說不定就能在火星水星金星木星土星海王星或天王星那充足而同的條件下生存下來。然而那個遠地點170的人類種族,盡管在方面與地球上的人類有著一定限度的不同之處,整個來說彼此卻有著的種種態。
  2. Volcanic rocks are characterized by wide distribution, complex lithology and lithofacies, and various eruptive forms. they are t ypically layer - or lens - like in shape and strike parallel to the principal structural lineaments in the region

    研究區火山巖分佈層位廣,巖性、巖復雜,噴發式多樣,呈層狀、層狀展布,延伸方向與區域線走向一致。
  3. Finally, in the third section, by constructing some functional which similar to the conservation law of evolution equation and the technical estimates, we prove that in the inviscid limit the solution of generalized derivative ginzburg - landau equation ( ggl equation ) converges to the solution of derivative nonlinear schrodinger equation correspondently in one - dimension ; the existence of global smooth solution for a class of generalized derivative ginzburg - landau equation are proved in two - dimension, in some special case, we prove that the solution of ggl equation converges to the weak solution of derivative nonlinear schrodinger equation ; in general case, by using some integral identities of solution for generalized ginzburg - landau equations with inhomogeneous boundary condition and the estimates for the l ~ ( 2 ) norm on boundary of normal derivative and h ~ ( 1 ) ' norm of solution, we prove the existence of global weak solution of the inhomogeneous boundary value problem for generalized ginzburg - landau equations

    第三部分:在一維情,我們考慮了一類帶導數項的ginzburg ? landau方程,通過一些類於發展方程守恆律的泛函及巧妙的積分估計,證明了當粘性系數趨于零時, ginzburg ? landau方程的解逼近應的帶導數項的schr ( ? ) dinger方程的解,並給出了最優收斂速度估計;在二維情,我們證明了一類帶導數項的廣義ginzburg ? landau方程整體光滑解的存在性,以及在某種特殊情下, gl方程的解趨近於應的帶導數項的schr ( ? ) dinger方程的弱解;在一般情下,我們討論了一類ginzburg ? landau方程的非齊次邊值問題,通過幾個積分恆等式,同時估計解的h ~ 1模及法向導數在邊界上的模,證明了整體弱解的存在性。
  4. The western hubei - eastern sichuan area is located at the junction belt between the eastern sichuan folded belt in the sichuan basin and xianexi folded belt, belong to eastern extended part, which is similar to the eastern - sichuan structure in many aspects. for example, they share a structural unit, resulting in the same sedimentary history and the same generation - reservoir - seal assembly as each other

    鄂西渝東區處於四川盆地川東褶皺帶與湘鄂西褶皺帶的接合部位,屬川東褶皺帶東延組成部分,具有與川東的沉積發育史與生儲蓋組合;同的發育史與式;類的天然氣藏類型與保存條件。
  5. This paper summaries ten basic tectonic type and similar thirteen kinds of tectonic forms according to different combination of tectonic forms and structure, combined with the characteristic of fault kinematics

    根據態和不同類型的組合關系,結合斷層運動學特徵,總結出10種基本類型以及與其的13種態。
  6. The key factors to make the slide is controlled to make the model be similar in geometry, material and fabric with the antetype, then simulate the infection of river, digging of road and so on, measure the data of the distortion of model, analyze the reason of the distortion and factors of the slide

    試驗抓住成滑坡的主要因素,根據所得的巖石力學參數及結面參數,在幾何條件、模型材料、結面條件等方面都基本滿足原理的情況下,對模型進行了河流下切、公路開挖等條件的模擬,測量觀察邊坡的卸荷回彈與層面的彎曲變情況,利用所側數據分析論證滑坡的成機制和影響因素。
  7. In the high - resolution seismic profile, to directly identify the diapir is often difficult due to much similarity between diapir and the invasion of igneous rock, thus leading to multi - resolution

    在高解析度地震剖面解釋中,直接識別泥底辟存在一定困難,主要因為泥底辟和火成巖侵入體在態上十分,容易成解釋的多解性。
  8. Using the theories of probability, algebra and number theory comprehensively, we investigate a class of boolean functions with three - valued walsh spectrum in the first part of this dissertation : the properties of the extended semi - bent functions, which are constructed from any two bent functions, are studied, followed by the structure characteristics of the boolean functions satisfying propagation criterion with respect to all but two vectors ; the definition and cryptographic properties of k - order quasi - bent functions are proposed whose walsh spectrum takes on only three values. some sufficient and necessary conditions are offered to decide whether a boolean function is a k - order quasi - bent function ; a special method is presented to construct the k - order quasi - bent functions, whose cryptographic properties are explored by the matrix method, which is different from the method of walsh spectrum and that of autocorrelation of boolean functions ; the application of this kind of boolean functions in the fields of stream cipher, communications and block ciphers is discussed, which shows the great importance of the fc - order quasi - bent functions ; some methodology are proposed to construct the k - order quasi - bent functions, including the complete construction by using the characteristic matrices of boolean functions, and the recursive method by two known k - order quasi - bent functions we further extend our investigation to the ring zp, where p is a prime, and the similar results are presented as far as the p - valued quasi - generalized - bent functions are considered

    本文首先綜合運用概率論、代數學、數論等基礎學科的理論知識,並以頻譜理論作為主要研究工具,對一類譜值分佈對均勻的函數? ?廣半bent函數、 k階擬bent函數和p值k階擬廣義bent函數進行了系統、深入的研究,給出了廣半bent函數定義,並探討了廣半bent函數的密碼學性質;給出了k階擬bent函數和p值k階擬廣義bent函數的定義及等價判別條件;討論了k階擬bent函數和p值k階擬廣義bent函數與部分bent函數和p值廣義部分bent函數的關系,探討了它們的密碼學性質;給出了k階擬bent函數和p值k階擬廣義bent函數的典型方法,並將對k階擬bent函數的密碼性質的研究轉化到對一類特殊的矩陣的研究上;利用布爾函數的特徵矩陣原則上給出了k階擬bent函數的一種完全方法,還給出了從已有的p值k階擬廣義bent函數出發,遞歸變元個數更多的p值k階擬廣義bent函數的方法;初步探討了k階擬bent函數在序列密碼、分組密碼以及通信中的應用;給出了一類布爾函數walsh譜的分解式,並利用這類布爾函數的walsh譜分解式給出了一類近穩定的布爾函數的,特殊情下為k階擬bent函數;利用代數數論的知識考察了p值k階擬廣義bent函數的譜特徵,並給出了k階擬廣義bent函數與所有仿射函數的符合率特徵等等。
  9. Fractal dimension structure form of the cosmos are explored, and the mathematical foundation, which include the expressions of fractal dimension differential and calculus, regular space integral solutions of fractal dimension differential equations, the fractal calculus definitions of fractal measure as well as the measure computational equation of self - similar fractal, of fractal dimension calculus and fractal measure are given

    摘要探討了宇宙分維式,給出了分維微積分及分測度的數學基礎,包括分維導數及分維微積分的表述式、分維微分方程的規整空間積分解、分測度的分維微積分定義及自的測度計算方程。
  10. For the purpose of improving calculation precision and reduce workload, viscoelastic similar shape element is generated in the numerical research about crack problem, using the characteristic of similar stiffness matrix between element near crack tip

    在裂紋問題的數值研究中,為了提高計算精度、減輕計算工作量,了粘彈性界面單元,利用裂尖附近單元剛度陣的特點,採用聚縮法成裂尖超級單元。
  11. In the paper, on the basis of expounding the importance of similarity theory in the numerical simulation of tectonic stress field, it is pointed out that, only by making the numerical model be similar to the geological prototype in material, combination pattern, boundary condition, loading mode and cracking criterion, etc., may the simulation result be real

    摘要論述了在應力場模擬中性原理的重要性,指出地質原與數值模型在材料、組合式、邊界條件、受力方式和破裂準則等方面必須,模擬的結果才具有真實性。
  12. It is very resembly representative island arc volcanic rock in the geochemistry character, so i demonstrate that a petrofabric formed tectonic activity section and island arc environment ; i also demonstrate that parametamorphite in the a petrofabric formed tectonic activity section. b petrofabric is very resembly a petrofabric in many aspects, so i think that b petrofabric also formed island arc environment, but volcanic activity obvious weakened in the b petrofabric stage. c petrofabric formed carbonatite mesa

    在地球化學特徵方面與典型島弧火山巖非常,得出a巖組成於活動區,成環境為島弧環境。 a巖組的副變質巖的原巖碎屑巖是快速堆積的,處于活動區。 b巖組和a巖組對應的巖石在各個方面都非常,所以成環境也為島弧環境,只是火山活動在這期間明顯減弱。
  13. Main works : fractal and mechanism of forming fractal of fault surface in rock masses is analyzed and examined with it ' s affect on failure process of mining rock masses ; fractal curves are constructed with matlab to simulate the fault surface. similar material modeling is carried out and the fractal weak - face effect of mining rock masses is studied. mechanics character of rock masses with fractal fault in mining condition is simulated with large finite element software an sys ; catastrophe model of fault activated by mining is constructed with catastrophe theory

    主要工作有:檢測和分析了巖體斷層面的分性和斷層面分成機制及其對采動巖體破壞的影響機理;運用matlab了分曲線來模擬分斷層面,進行了材料模擬實驗,研究了采動巖體的分弱面效應;採用大型有限元軟體ansys模擬了含有分斷層面的巖體在采動條件下的力學性態;運用突變理論建立了采動斷層活化的突變模型。
  14. 2. the feature of geochemical primary halo in longshujiao ore segment shows that there is a positive abnormality of fi set of main chemical elements at 96 ~ 100 investigating line, longshujiao fault and fault 11 - 29, a east - north a positive abnormality of fs set of main chemical elements around 98 investigating line, big area positive abnormality of f4 set of main chemical elements in east ore segment and the feature of this abnormality is like the shape of the main ore - body in the west

    2 、龍樹腳礦段原生暈特徵分析顯示, f _ 1主元素因子組在96 100勘探線,龍樹腳斷裂至? 29號斷裂間出現一個因子得分高值異常; f _ 5因子組以98勘探線為中點,因子得分值成一個北東向高值異常; f _ 4因子組元素因子得分在東礦段成大面積異常區,異常特徵與西部主礦體地表展布
  15. Based on the contrast of the comparability, the paper concludes that the footwalls of reverse faults in the front of altun mountain may form effective hydrocarbon traps

    通過對比分析兩者之間的性,認為柴達木盆地阿爾金山前帶深部發育的逆沖斷裂下盤也應該具有成油氣圈閉的條件。
  16. Situated at the both e w sides of pamir, the s w tarim and tadjik basins have the similar evolution history of tectono sedimentary processes during cenozoic, i. e. steady subsidence with transgressive sequence in paleogene and speedy subsidence with continental molassetype sediments in strong compressive tectonic environment in neogene - quaternery. since neogene, for the effect of pamir and west kunlun s northward moving and thrusting, there is complicated tectonostructural deformation taking place in tadjik and sw tarim. neogene stratigraphic combination and later structural deformation of tadjik basin and southwestern tarim much resemble each other in terms of extent of transpressional processes. paleogene in tadjik basin is main oil - bearing sequence and many substantial oil - gas fields there have been found. so, it can be assured in comparison that there is oil - gas perspective also in southwestern tarim region

    第四紀受強烈擠壓快速沉降接受陸磨拉石沉積。自新第三紀以來,受帕米爾西昆侖北移和隆升沖斷的影響,塔西南和塔吉克盆地發生了復雜的褶皺沖斷變,其差異在於塔西南明顯地受走滑為主的剪壓作用,而塔吉克盆地是受擠壓為主的剪壓作用的影響。塔西南和塔吉克盆地下第三系巖組合類,後期,塔吉克盆地下第三系是該盆地的主力油層,已有許多油氣田發現,因此可以推斷塔西南也應該有良好的油氣前景。
  17. Generally the fractal is regarded as the aggregate state of the big and small fragments and the fractal is a general name to those without characteristic length, including the graphics, structure and phenomena. it is said that the fractal is a figure whose composed parts look like their whole by a certain mode

    一般把分看作大小碎片聚集的狀態,是沒有特徵長度的圖以及現象的總稱。也可以說,組成部分以某種方式與整體體叫分。分的兩個重要特徵是自性和標度不變性。
  18. It is difficult to demand the geological structure patterns physical model to whole satisfy the similar condition, because geometric dimension of geological structure is immense, its elapsed time is too long and its structure deformation is considerably complex ; therefore, the people are not satisfied with the results of geological structure physical modeling experiment yet

    由於地質尺度的宏大,經歷的久遠和變的復雜性,地質物理模型設計時幾乎不可能完全滿足原理的適用條件,因此,各種地質物理模擬實驗還不十分令人滿意。
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