構造樣式 的英文怎麼說

中文拼音 [gòuzàoyàngshì]
構造樣式 英文
structural pattern
  • 構 : Ⅰ動詞1 （構造; 組合） construct; form; compose 2 （結成） fabricate; make up 3 （建造; 架屋） bui...
  • 造 : Ⅰ動詞1 （做; 製作） make; build; create; produce 2 （假編） cook up; fabricate; concoct 3 [書面語...
  • 樣 : Ⅰ名詞1. （形狀） appearance; shape 2. （樣品） sample; model; pattern Ⅱ量詞（表示事物的種類） kind; type
  • 式 : 名詞1 （樣式） type; style 2 （格式） pattern; form 3 （儀式; 典禮） ceremony; ritual 4 （自然科...
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  • 樣式 : pattern; type; style; form; model; modality; genre
  1. Tectonic styles and oil - gas distribution in yitong graben

    伊通地塹構造樣式及其油氣分佈規律
  2. And its special tectonic conditions contribute to the development of the deep - thick - incompact slopes growing in badong formation

    三峽庫區位於大巴山弧形構造帶與八面山弧形構造帶的接合部，構造變形強烈，構造樣式多樣。
  3. The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang, which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw, came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin, i. e. the strike - slip and stretch processes of baigezhuang fault

    同時，用三維地震資料進行區域構造解釋分析，論述了柏各莊地區的構造樣式，是中新生代渤海灣裂谷盆地的幕斷陷發育階段，同時由於盆地內凸起邊界?柏各莊斷層的走滑兼伸展作用，使柏各莊凸起的中生界形成壘、塹斷塊群構造樣式，發育一系列ne （ nee ）向，傾向nw或sw的正斷層。
  4. The main structure style of chagan sag included four kinds, such as extension, compression, inversion and strike - slip structure, in which the extension structure was the principle part

    查干凹陷的主要構造樣式包括伸展、擠壓、反轉和具有走滑分量的構造，其中伸展構造是主體。
  5. B - 3 spline and reversed b - 3 spline is adopted to construct the outer figure of fashion parts. the key points are also defined to support the rigging of fashion parts. the two main modules - style input module and the intelligent rigging module are also described in details

    採用三次b樣條曲線和反算三次b樣條曲線來構造款式部件的外輪廓；定義部件關鍵點支持部件的拼接；對構成智能款式設計的兩大模塊?款式輸入模塊和智能拼接模塊，給出了設計要求和實現效果。
  6. Yanqi basin, located in the northern wing of the " v - type " thrust - fold belt, is related to the reversion of the kuluketage aulacogen

    因此庫魯克塔格裂陷槽的構造反轉是焉耆盆地構造變形的主要力學來源。 2 、描述了盆地內的構造樣式。
  7. Different tectonic style exists in the upper and lower layers of the yanshanian boundary. the lower layers takes on the tectonic style of thrust fault and nappel. the upper layers hi step positive fault

    2 、盆地燕山期構造界面上下不同構造層具有完全不同的構造樣式，構造界面下伏構造層呈現沖斷褶皺、推覆構造樣式，構造界面上覆構造樣式為階梯狀正斷層，整體呈現「雙層」結構型式。
  8. The structural style ; thrust ; kongxi structural belt

    構造樣式逆沖構造孔西構造帶
  9. The tectonic style inside the basin is characterized by occurrence of anticlines from the margins to center of the basin, with two limbs mostly starting from reverse faults, developing a tectonic pattern of two faults sandwiching an uplift

    盆地內部的構造樣式以自盆地邊緣至中心以此形成背斜構造為顯著特徵，背斜兩翼多發育逆斷層，構成「兩斷夾一隆」的構造格局。
  10. Analysis on structural style in the hailaer basin

    海拉爾盆地構造樣式分析
  11. Impact of geometry and kinematics of lanliao fault on structural styles in dongpu sag

    運動學特徵對東濮凹陷構造樣式的影響
  12. September 2002. see how the websphere studio tools can assist in the development of xslt style sheets by taking the

    ， 2002年9月） ，了解構造樣式表的不同方法。
  13. 8. it is concluded that three entrapment models likely exist, a model on the steep slope, a model on the gentle slope and a model on the horst between the two depressions by

    8 、研究有利區帶構造樣式及其油氣關系，認為可能存在三種成藏模式即陡坡帶的成藏模式、窪中壘成藏模式和緩坡帶成藏模式。
  14. The structure units are redivided. the main structure style of chagan fault depression is summarized, in which the extensional structure are the principle part. its kinematics characteristics are analysed

    對查干凹陷的構造單元重新進行了劃分，總結了查干凹陷的主要構造樣式，伸展構造是主體，並對其運動學特徵進行了分析。
  15. At last they have being formed the tectonic framework, after breakup of the volcanic island arcs, subduction, decline and fall of the back - arc basins and arc - microcontinent and arc - arc collision had finished

    經過了長期而復雜的微大陸和火山弧的裂解、弧后盆地的消減衰亡及弧陸和弧弧碰撞等構造演化，才最終形成今天所見到的這種構造樣式。
  16. Combined with geologic condition and infrastructure characteristics, balance three great structure profiles which trend sn with balance profile theory, then analyze the structure style, association form and each detachment further, and calculate 30 % shorten after the stratum deformation variant it turns out to be striking detachment in multiple tectonic levels and different structure deformation variant style in different stage, after the discussion of the structure style and relation between infrastructure and suprastructure

    結合地表地質情況和深層構造特徵，利用平衡剖面原理對三條地質構造剖面進行了平衡，通過平衡后的剖面更好地對剖面所反映出的構造樣式、組合形態及各個滑脫面進行分析，並且計算出變形后地層的變形縮短量為30左右。研究區內深淺層構造之間存在著顯著的多層次滑脫，且不同層次上構造變形樣式各不相同。
  17. Based on the four geologic structural section ( 2 pieces ne - sw direction, 2 pieces nearly ew direction ) which controlled different structural area and several supplementary profiles and several other auxiliary sections, summarize and analyze the structural style research area. surface structural styles shown on great profiles were discussed in different structural section after continual observation

    以野外測制的控制不同構造區的四條地質構造剖面（北東-南西向兩條、近東西向兩條）及若干輔助剖面為基礎，對研究區的構造樣式進行了總結和分析。
  18. Based on predecessors research by geological - geophysical synthesized studying and three - dimensional technique, draw up west, middle and east three composite profiles, explanation of the structure model in different level including surface, middle and deep of the basin, finally concluded in homogeneity of the basin is show by belting in south - north trend, block - faulting in east - west trend and vertical sphere - laying

    在前人研究基礎上，採用地質-地球物理綜合研究和三維技術，編制了西、中、東部三條地學綜合剖面，研究解釋了盆地淺、中、深部不同層次的結構構造樣式，得出盆地地殼結構不均一性規律。
  19. The three gorge reservoir, locating at the suture between two arc tectonic belts of daba mountain and bamianshan, has strong structural deformation and versatile structural patterns

    摘要通過分析大量資料並結合野外地質工作，對三峽庫區的區域構造背景及巴東組的主要構造樣式進行了總結，分析了這些地質要素對三峽庫區變形斜坡形成和發展的影響。
  20. The extending major fault has a strike of north - east, controlling the forming of depressions and evolution of sedimentation. the nature of the fault is normal in the early stage. later with the reformation of sliding effect, normal faults are still the main faults, and the plane distribution of the faults occurs sectionally

    取得了一系列的研究成果：遼河灘海地區主要有三種構造樣式，即伸展構造樣式、走滑構造樣式及反轉構造樣式，其中，以伸展構造樣式為主，伸展主幹斷裂走向以北東走向為主，控制凹陷形成和沉積演化，斷裂性質早期為正斷層，後期經走滑作用改造，至今仍以正斷層形式出現，斷裂平面展布具有分段性。
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