斷裂結構 的英文怎麼說

中文拼音 [duànlièjiēgòu]
斷裂結構 英文
fracture structure
  • : Ⅰ動詞1 (分成段) break; snap 2 (斷絕;隔斷) break off; cut off; stop 3 (戒除) give up; abstai...
  • : 裂動詞[方言] (東西的兩部分向兩旁分開) open
  • : 結動詞(長出果實或種子) bear (fruit); form (seed)
  • : Ⅰ動詞1 (構造; 組合) construct; form; compose 2 (結成) fabricate; make up 3 (建造; 架屋) bui...
  • 斷裂 : break; disrupt; flying off; fracture; fragmentation; out break; rift;crack;bursting;rupture;rendi...
  • 結構 : 1 (各組成部分的搭配形式) structure; composition; construction; formation; constitution; fabric;...
  1. In the tide of the afflux of knowledge from west to east, with the transplantation of modern legal system, development of legal education and the introduction of the western legal analysis method, both the legal system and the legal knowledge system of classical china ruptured, then collapsed

    隨著西學東漸,隨著現代西方的法制、法律教育與法學研究範式的全面導入,古典中國的法律制度與法律知識體系開始出現,並且迅速解體。
  2. It is barely ten since systematic deep ocean bathymetry revealed the structure of rifts, fractures and trenches associated with sea floor spreading.

    系統的深海深度測量揭示了與海底擴張有關的狹谷帶、帶和海溝的
  3. When the rock mass of dam abutment is enclosed by faults, joint fissures and bedding planes, it is necessary to carry out holistic anti - slide stability analysis in order to make the abutment withstand potential slide

    摘要當拱? ?肩巖體為層、節理隙、層面等面所圍成,有可能產生滑移時,就應進行整體抗滑穩定分析。
  4. Stability of rock slopes is generally controlled by the structure of rock masses, especially the soft structure surfaces. analysis of rock mass structures is a key to establish geological models and numerical simulation and a foundation to assess the stability of rock slopes. the weak structure surfaces are mainly bedding planes, faults, joints, schistosity plane and contact zones of intrusive bodies. since they are different in genesis and scale, the rock masses are different in features and mechanical intensities. based on the combination of rock structure bodies, 15 basic modes of deformation and failure of rock slope are systematically summarized. the deformation and failure of rock masses actually result from the recombination and rearrangement of these rock bodies. there are 11 types of rock mass structures and various deformation and failure of bank slopes are present in the reservoir area of the three gorge project

    巖體,特別是軟弱面對基巖斜坡變形與破壞具有顯著的控製作用,巖體模式分析是建立斜坡地質模型和數學模型的關鍵和評價斜坡穩定性的基礎。巖層層面造節理隙片理與劈理以及侵入體和圍巖的接觸帶等是控制基巖斜坡穩定的軟弱面,這些成因不同大小不一的面將巖體分割成性質各異力學強度不均的各種巖體體,成了15種基巖斜坡變形破壞的巖體基本模式。不同體的重新組合與排列是斜坡失穩的內在原因。
  5. Three stages of deformation can be distinguished from the cataclastic superposition of matrices that infilled the microcracks in cataclastic rocks, and two phas es of paleotectonic stress field from the typical conjugated shear joints by stereograms illustrating

    造巖中膠物和微隙充填脈反映了巖石碎變形的三次疊加。變形帶內發育兩期典型的共軛剪節理,但區域分佈各有特點,反映出變形的空間演化。
  6. ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin

    ( 6 )論文探討了賽什騰? ?錫鐵山斜向逆沖推覆造的地質意義,認為賽什騰-錫鐵山斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的果,該認識對于研究柴北緣區域造格局、盆山關系以及更大尺度的帶或造山帶的斜向逆沖作用具有理論意義,對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。
  7. The ultrastructure of the merozoites of eimeria tenellawas observed and discribed. the pellicle consist of two layer membranes, the outer membrane was a continous covering enclosing the whole merozoites, while the inner pellicular complex is interrupted at the anterior and the micropore, and thicken to form the polar ring and micropore. there are 24 microtubules under the pellicle of the merozoite which originated from the polar ring, all of them are connected with the polar ring, and extend alongside the inner pellicular complex to the middle of the merozoite. the head of the merozoite consists of a conoid, an apical vesicule and polar ring. the conoid is a hollow truncated cone. the conoid and spical vesicule can stretch and contract. there are three or more rhoptry and a lot of micronemes. the nucleus has nucleolus. and two layer membranes

    利用透射電鏡對柔嫩艾美耳球蟲殖子的超微進行了觀察描述.柔嫩艾美耳球蟲殖子的表膜由外膜和內膜復合體兩層組成,外膜連續,內膜復合體在頭部開形成極環,在其它部位開形成微孔;殖子的膜下微管24根,起始於極環,向後延伸至細胞核處;殖子的頭部由頂泡、錐體和極環組成,錐體和頂泡可以伸縮;柔嫩艾美耳球蟲殖子棒狀體3個以上,微線數量很多,二者都由電子緻密的組成;細胞核位於殖子的中後部,外被雙層膜,有電子緻密的核仁和染色質
  8. In spermatogenous cell, we could find dilated cytolemma, dilated nuclear membrane and fused crista of mitochondria. most of the sperm ' s cellular membrane dissolved and broke down into pieces. the central granule and mitochondrion showed little dissolving

    久效磷可以使金魚精子細胞質膜溶解,出現間;有的精子頭部變形,頂部出現凹陷;少量精子頸部中心粒復合體溶解;精子頸部線粒體有溶解現象,精子尾部的膜
  9. At low concentration of zn, the changes in ultrastructure were nuclei deformation, chloroplast swelling and disorder of thylakoid arrangement ; serious damages in ultrastructure caused by greater zn stress were indicated by scattered nucleoli, condensed chromatin, almost empty nuclei with nuclear membrane disrupted and nucleoplasm flowing into cytoplasm, swollen and partly dissolved cristae of mitochondria, disrupted and collapsed chloroplast envelopes, and some dissolved thylakoids that flew into cytoplasm

    超微的變化也呈現加重趨勢,低濃度處理的變化為細胞核變形、葉綠體膨脹、類囊體排列紊亂;嚴重的超微的損傷是核仁散開、染色質凝集,細胞核幾乎成為空核和核膜破,核質散出;線粒體脊突膨脹和部分溶解;葉綠體膜、消失和部分類囊體溶解和散到細胞質中。
  10. On the basis of detailed field work and structural analysis, this paper presents a new geometrical and kinematic data that reveal the staictural characteristics of qinglong fault zone. this fault zone is composed of numerical ew faults with an arrangement of dextral step pattern in the western part, and consists of maquanzi - datun fault and tumenzi - mingshui fault in the eastern part

    本文通過較為詳細的野外調查和室內研究,並合前人的研究資料,以造解析為指導思想,對帶的幾何學、運動學特徵進行了研究:青龍帶是由一系列近東西向的層組合而成,帶西段呈明顯的右行右列式分佈,東段主要有馬圈子?大屯和土門子?明水組成。
  11. Sxotf is recognized in the northern qaidam based on the analysis of structures of area. this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge, fault breccia and fault cleavage. fault hanging wall consists of sertengshan - xitieshan napple, which is distribution in dextral en echelon. fault footwall consists of youcangshan formation in neogene

    本文在對賽什騰? ?錫鐵山斜沖詳細地段造解析的基礎上,合盆地的沉積特徵、地球物理資料等對該斜沖的幾何學、運動學及形成時代進行了研究,論文著重探討了賽什騰? ?錫鐵山斜沖的地質意義。
  12. Especially interesting is the serpentinous peridotite in this belt occurred as lense blocks of various sizes, and superimposed with other geological masses with faults, and in combine to constitute the mixture. system in the belt. five tectonic stage can be discerned in this area : ( 1 ) south - north ward overthrust ; ( 2 ) sinistral strike - slip ( 3 ) dextral strike - slip ( 4 ) south - north ward overthrust ( 5 ) northeast, northwest late stage fault

    本區上述的造特徵先後經歷了五期造作用,依次為: ( 1 )南北向逆沖推覆; ( 2 )左行走滑; ( 3 )右行走滑; ( 4 )南北向擠壓推覆; ( 5 )北東向、北西向晚期
  13. An obvious split appears in the social interests structure due to the fact that the old social interest distribution has not been broken and the new one hasn ’ t established, hence the social interests have kept being disunited and being integrated and the conflicts among the interest groups are on a rise

    由於舊的社會利益格局被打破,新的社會利益格局還沒有定型,社會利益出現了明顯的痕,社會利益不分化整合,利益沖突也出現出加劇的趨勢。
  14. The results of 2 - d resistivity inversion of the yishui - tangtou and the liujazhuang faults indicate that electrical structures on both sides of the fault zone present obvious difference, the resistivity of the hanging wall is low and partially high, while that of the foot wall is high, and the faults are high - obliquity faults

    沂水湯頭、劉家莊的二維電阻率反演果表明,帶兩側的電性呈現出整體性的差異,正層的上盤為低阻區和局部高、低阻擾動區;而層下盤多為均勻的高阻區;層為高角度層。
  15. Fracture is not the only way that a structure can fail.

    並非失效的唯一形式。
  16. Most damage of construction is due to the crack, so people always consider the beginning of crack as the sign of danger, it always makes people fear. with the development of economy in our country, the dimensions of construction is larger and larger, and the engineering is growing towards large - scale and complexity, because the refresh of material of concrete, the strength of concrete is improved, but a lot of crack appears in the engineering. in recent years, as the further development of economy in our country, the need of steel in the engineering is increscent, but the supply of steel in our country can not satisfy with the need, the price of steel is continuously rising, so it gives us a problem, we must save steel in designing construction and simultanentily controlling the crack of construction. so it gives us a new question on crack study

    由於建築物的破壞往往始於縫,所以人們一般把縫的出現視作危險的徵兆,縫使人們產生恐懼感。隨著國家經濟的發展,工程建設規模越來越大,工程朝著大型化、復雜化的方向進展,隨著混凝土原材料的不更新,混凝土強度等級的不提高,在實際工程上出現了大量的縫問題。近年來隨著國家經濟的進一步發展,用於工程建設的用鋼量日趨增大,而國家的鋼材供應量不能滿足日趨增大的市場需求量,導致鋼材的價格不上漲,這就要求我們在節約鋼材用量的基礎上來設計控制工程中的縫問題,這也就給縫研究提出新的課題。
  17. I. a mtil ( iaxial elastic - plastic hardening - sofling constitutive model of concrete is proposed iii order to offer a nonlinear material model of concrete for space restoring force analysis of reinforced concrete members taking into account the softening behavior of concrete. the concrete material model is incorporated the elastic - plastic hardening fracturing constitutive model of concrete with the plastic - fracturing theory of concrete, modified without defining two loading functiomis, and based on five parameter power function failure criterion proposed by guo zheng - hai etc from tsingliua ( jniversity, or three parameter unified strength theory proposed by yu mao - hong from x ian iiaotong university

    1 、將砼彈塑性硬化模型與塑性理論合起來,並加以改進,但無需定義兩個加載面,以清華大學過鎮海建議的五參數冪函數或以西安交通大學俞茂宏建議的,參數統一強度理論作為砼的強度破壞準則,建立了砼多軸彈塑性硬化松馳本模型,能為鋼筋砼件空間恢復力分析提供砼非線性材料模型,並能反映砼材料的軟化段。
  18. With topographic map and other methods, some class i v active faults that run through laohutai mine field in modern stress environment are found out by means of geodynamic zoning

    通過逐級使用地形測量圖並合其他方法查明了井田i v級活動,由各級所分割的展現出了井田現今造運動的果。
  19. Interaction between the city and the countryside in the market - oriented discontinuous structure

    市場主導型斷裂結構中城鄉互動
  20. The estimation for failure probability of brittle fracture structure

    脆性的失效概率計算
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