褶皺變形的 的英文怎麼說

中文拼音 [xízhòubiànxíngde]
褶皺變形的 英文
fold-modified
  • 褶 : 名詞（褶子） pleat; crease; fold; wrinkle
  • 皺 : Ⅰ名詞（皺文） crease; wrinkle; crinkle Ⅱ動詞（起皺紋） wrinkle up; crumple; crinkle; crease
  • 的 : 4次方是 The fourth power of 2 is direction
  1. This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible

    按照不同構造層，研究了各構造層的構造特徵：基底構造層：受早海西期構造作用的影響，與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關，為一構造變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層：受中海西區域性伸展斷陷作用的影響，盆地及其周緣地區發育與伸展構造有關的構造-巖漿組合，如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。
  2. They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill. we mark off five kinds of buried hill belts. they include three different kinds of trap on the basis of the cause of trap formation

    本次研究在重新認識濟陽坳陷區域構造背景的基礎上，將濟陽坳陷古生界潛山的形成過程分為四個階段，即古生代早中生代?穩定沉降?隆升?輕微褶皺變形及逆斷層發育階段、中生代?初步斷陷階段?塊斷期、新生代早期?斷拗階段?塊斷潛山形成期以及新生代晚期?坳陷階段?潛山定型期。
  3. Yili basin is a independent unit of the yili - zhongtianshan micro plate, which is subject to the zhunger - kazakstan plate. it is a superimposed basin which formed on the basis of the folded pre - permian basement, underwent rifting and breaking in permian, depressing and uplifting and multiple deformation and reformation after permian

    伊犁盆地是準噶爾?哈薩克斯坦板塊的一個次級構造單元?伊犁-中天山微板塊內的一個獨立單元，它是在前二疊紀褶皺基底的基礎上，於二疊紀擴張、裂解（谷） ，經二疊紀后的坳陷、隆升多期變形、改造而成的復合型改造盆地。
  4. Depending on the intensity of the deforming forces the folds may be gentle, sharp, overturned, or overthrust.

    根據變形力的強度，褶皺可以是平緩的，陡峭的，倒轉的，或逆掩的。
  5. It can be concluded that numerical simulation technology is a new method to analyze fold structure, and the method will find significant development in structural geology field

    數值模擬技術為褶皺變形提供了一種新的研究方法，該方法在構造地質領域將有很好的發展前景。
  6. The tectonism in this area can be divided into three phases, that is the folded basement formation and stable ancient land in pre - mesozoic, ancient land cracking phase in mesozoic, the faulted activity and subsidence phase in cenozoic

    本區構造變動劃分為三個大的階段，即：前中生代褶皺基底的形成和穩定古陸發育階段、中生代古陸裂解階段、新生代塊斷活動及整體沉降階段。
  7. By means of stress - strain feature of upper and lower strata of fold neutral plane in the course of longitudinal fold formation, the differences between the upper coal bed and lower coal bed of fold neutral plane are analyzed from the coal thickness, coal structure, coal body structure, coalbed gas occurrence and diversities etc., revealing the cause of these appearances

    摘要利用縱彎褶皺變形中中和面上下巖層的不同應力與應變特點，分析了處于褶皺中和面上下各煤層在背斜與向斜部位煤層厚度、煤層構造、煤體結構及煤層瓦斯的賦存規律與差異性，揭示了這些現象產生的原因。
  8. According to granite ages cutting ruptures, mineralized quartz veins ages corresponding to fold deformation and formation ages of bilateral faulted basin, deformation age are limited, that are 100 ~ 65ma for one and form 65ma to the present for two and three

    根據斷裂截切的花崗巖體年齡、同期褶皺變形的含礦石英脈年齡以及斷裂兩側斷陷盆地的形成時代，大致限定第1期變形時代為100 65ma ，第2 、 3期變形時代為65ma現今。
  9. The first phase involves the formation of thrusting and napping towards nww accompanied by extensive igneous activity and mineralization. the second phase corresponds to the development of asymmetrical small fold downwards north and south. the final phase the cenozoic is marked by strong brittle fractures activity resulting in the sharp heave of the landform of xiaoqinling aera

    太華群內的褶皺及南北兩側斷裂分析表明，小秦嶺燕山期至少經歷3期變形，第一期為sse nww向的褶皺變形作用；第2期為南北向正斷下滑剪切作用；第3期為脆性正斷作用。
  10. Because the structural interpretation of the 3d model only is of non - uniqueness and uncertainty due to geometric constraint, the finite strain analysis was also applied in the structural interpretation. 184 oriented samples have been drilled at 18 sampling sites in yanjinggou, western sichuan

    在川西鹽井溝地區18個采樣點鉆取了184塊定向巖心樣品，通過磁組構的分析結果發現，鹽井溝地區的磁組構基本上都是弱應變的初始變形組構，褶皺前翼應變強度比后翼略強。
  11. Two hours after her departure, i was still sitting on the bed she had just left, staring at the pillow which bore the imprint of her head, and wondering what should become of me, torn as i was between love and jealousy

    她走了已有兩個小時了，我還是坐在她適才離開的床上，凝視著床上的枕頭，上面還留著她頭形的皺褶，一面考慮著在我的愛情和嫉妒之間我將變成什麼樣子。
  12. We applied the new modifier skin morph to correct the deformations in the pleats

    我們運用了新的皮膚變形修改器去做皺褶的變形。
  13. The anatomy of small - scale to meso - scale deformational structures have resulted in the reconstruction of the structural framework of the yanbian group. the statistical analyses of the fold hinge and cleavages developed in the yanbian group suggest the trend of the first stage penetrating structures of the yanbian group is een - wws. 2

    基於對鹽邊群中、小尺度變形構造進行構造解析，建立了區域構造格架，通過對褶皺樞紐和劈理的分析，提出鹽邊群第一期透入性變形構造的走向為北東東?南西西向。
  14. The second part is load analysis. bases on the form - finding, the stress, strain and displacement etc are calculated under loads. also the problem of membrane drape and cable relaxation should be considered during this procedure

    第二階段是荷載分析階段，即找形分析獲得的曲面在各種可能荷載組合的作用下，求解其變形、位移、索膜內力及判別薄膜是否有褶皺產生或索是否有鬆弛現象。
  15. Based on our own simulation results and results of some numerical simulation of single fold structure by other investigators in recent years, the factors that affect single fold shapes and the variation of maximum principal stress and horizontal strain during the deformation of single fold are discussed in this paper

    本文結合近年來單層褶皺構造數值模擬研究進展，以及筆者近幾年來對單層褶皺所進行的數值模擬實驗研究，主要論述了單層褶皺變形的影響因素，單層褶皺變形過程中的最大主應力與水平應變的變化及其影響因素等。
  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相磨拉石沉積。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形，其差異在於塔西南明顯地受走滑為主的剪壓構造作用，而塔吉克盆地是受擠壓為主的剪壓構造作用的影響。塔西南和塔吉克盆地下第三系巖相組合類似，後期構造變形也相似，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. The style of deformation in different rock mass and tectonic units is varied. according to the distinction of stratigraphic assemblage, rock type. tectonic block type and the characteristics of deformation, the whole district can be subdivided into three structure belt. namely southern and northern metamorphic fold stratigraphic system and central tectonic mixed system and multi - stage intruded magmatites

    根據區內出露的地層、巖性、構造塊體、變形變質作用特徵，全區可分為南北兩帶的變質褶皺地層系統和中帶的構造混雜系統以及不同期次的巖漿侵入體。
  18. At first we made a white coat with many creases, but at the time of making the setup and deforming the mesh it was very complicated

    一開始我們就製作了白色外套和那些皺褶，但是在設置面片變形的時候非常的復雜。
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