坡折 的英文怎麼說

中文拼音 [pōzhé]
坡折 英文
break in grade
  • 坡 : Ⅰ名詞（地面傾斜的地方） slope Ⅱ形容詞（傾斜） sloping; slanting
  • 折 : 折動詞[口語]1. （翻轉） roll over; turn over 2. （倒過來倒過去） pour back and forth between two containers
  1. It can roar through the leafless oaks and shout down the hillside, and it can murmur in the white pines rooted among the granite ledges where lichen makes strange hieroglyphics

    它在山坡呼嘯著光禿的櫟樹，它在植根于布滿曲折青苔花崗巖的五針松下低語。
  2. They entered the woods, and bidding adieu to the river for a while, ascended some of the higher grounds ; whence, in spots where the opening of the trees gave the eye power to wander, were many charming views of the valley, the opposite hills, with the long range of woods overspreading many, and occasionally part of the stream

    他們走進樹林，踏上山坡，跟這一灣溪流暫時告別。從樹林的空隙間望出去，可以看到山谷中各處的景色。對面一座座小山，有些小山上都長滿了整片的樹林，蜿蜒曲折的溪流又不時映入眼簾。
  3. At last, the finite element method, the strength reduction method and limit equilibrium method, nature slopes and excavation slopes, lateral stress unloading model and axial loading model are analyzed and discussed relatively

    最後，就有限元法、強度折減法和極限平衡法，自然邊坡與挖方邊坡，圍壓卸荷應力路徑模型分析與軸向加荷應力路徑模型分析進行了比較討論。
  4. The narrow road is on a gentle slope which occasionally makes sharp twists.

    這條狹路是在一個平緩的斜坡上，它有時曲折得很厲害。
  5. In this paper, based on the analysis of the rlem of theory foundation, computing method, preference, applicability, etc, we anatomized the rlem of three self - deficiencies and six scarcities. moreover, we adopted the parallel ways of contrasting the rlem with the fem and applied it to analyzing the impact of slide block of elasticity and plasticity, slip surface of coefficient and slip bed of elasticity, plasticity upon the stability of slope and in the plain linearity slope, the plain refracted line slope and the plain arc slope. in addition, we discussed the warp of between the lem of ( sarma, janbu, order, bishop, morgenstera - price, etc ) and the fem of result and the distributing of positive stress and shear stress on the slip surface

    本文從剖析剛體極限平衡法的理論基礎、計算方法、參數選取、適用條件等方面入手，剖析了剛體極限平衡方法的3點自身缺陷和6點不足，並在此基礎上採用了剛體極限平衡法（平面滑動破壞法、 sarma法、傳遞系數法、普遍條分法、 janbu法、 bishop法、 morgenstern - price法）與大型有限元法對比研究的方法，分析研究了平面直線型滑坡、平面折線型滑坡、平面圓弧型滑坡在漸進破壞中邊坡的滑體彈塑性參數、滑麵塑性參數） 、滑床的彈塑性、以及極限平衡法無法考慮開挖應力釋放等因素對邊坡穩定性的影響與滑動面上的正應力、剪應力分佈規律、安全系數的解答的差異。
  6. It is therefore proposed in this paper to strengthen the exploration of such wide and deep subsags as chagannuoer and hongqi subsags, to lay emphasis on the exploration of superposed and residual fault depression, and to pay attention to the discovery of various oil and gas reservoirs including metamorphic buried hills, fracture slope breaks, and volcanic rocks, etc

    因此，指出下一步應加強類似查干諾爾，紅旗等寬深窪槽的勘探，重視具疊合型和殘留型斷陷的勘探，注重尋找包括變質巖潛山，斷裂坡折帶、火山巖等在內的各類油氣藏。
  7. Study on slope breaks of the late cretaceous depression basin around the western slope in the southern songliao basin

    松遼盆地南部西部斜坡區晚白堊世坳陷盆地坡折帶研究
  8. Types of the paleogene slope - break zones and distribution of the subtle traps in gaoliu area of nanpu sag

    南堡凹陷高柳地區古近系坡折帶類型及隱蔽圈閉分佈特徵
  9. This thesis predict profitable oil trap under the direction of the theory on searching for oil in faulty - step break, and select classy from them in terms of the style, scale, reservoir factor and shelter of the sedimentary sand - body distributing. take the low stand system of down - shasan formation for example, three favorable targets was put forth through synthesis analysis

    本文在斷階坡折找油理論的指導下，對研究區內的有利圈閉進行了預測，並根據沉積砂體的分佈類型、規模、儲層物性以及封堵條件，再結合現有鉆井的試油分析情況，對其進行優選，以沙三下段低水位體系域為例，經過綜合分析，提出了3個有利的目標。
  10. Near the faulty step - break, low stand system developed, and some sediment system distribute broad, such as alluvial fan, low stand wedge, low stand fan, and so on. the sand body can form not only the trap of dying out upward and sand lens, but also fault - iithology trap. the study shows that fault - lithology trap is most important trap style in study area especially sha - 3 formation

    斷階坡折附近是低水位體系域發育的重要場所，常發育沖積扇、沖蝕作用的下切河道以及低水位楔狀體、低水位扇體等沉積體系，這些砂體不僅具有形成上傾尖滅或砂巖透鏡體圈閉的條件，而且可形成斷層?巖性圈閉。
  11. Fault break - slope and low - stand fan sequence in dongying sag

    東營凹陷深陷期構造坡折帶與低位扇序列
  12. Origin of lowstand fan in faulted - topographic break amp; play ' s characteristics

    斷裂坡折帶低位扇成因及成藏特徵
  13. Reservoir - forming conditions in fault slope break at the margin of dongzhuang sub - depression

    東莊次凹邊緣斷層坡折帶對油氣成藏的作用
  14. Genetic types of paleogene slope - break zones and their controls on depositional system in bohai offshore

    渤海古近系坡折帶成因類型及其對沉積體系的控製作用
  15. Arc - shaped fault break slope system and its control on low stand systems sandbodies in dongying depression

    東營凹陷弧形斷裂坡折帶系統及其對低位域砂體的控制
  16. Patterns of the slope - breaks in bamianhe area of dongying sag and the controls of the slope, breaks on subtle traps

    東營凹陷八面河地區坡折帶特徵及其對地層巖性圈閉的控製作用
  17. In this condition, applying the theory on searching for oil in faulty - step break to direct exploration must acquire good effect

    針對這種斷層控制的地層發育狀況，在工區應用斷階坡折帶找油理論來指導勘探，必將取得良好的效果。
  18. The knowledge about slope break belt is put forward, it is point out that the slope break belt in kenxi area is the controlling factors of oil - gas distribution and reservoir forming by enrichment, it is is favorable zones of exploration in the future

    並提出了坡折帶這一新認識，文章指出波折帶是墾西地區油氣分佈與富集成藏的控制因素。墾西地區波折帶是下步勘探的有利區帶。
  19. The structural slope - break zones are defined as the depositional slopes abrupt change in geomorphology and developed widely in fault and foreland basins, the recognition of which is significant for predicting the distribution of depositional systems tracts, particularly the lowstand systems tracts which usually comprised economically important reservoirs in these basins

    構造坡折帶是由構造活動所產生的、對沉積作用具有長期控製作用的古沉積斜坡或古地貌突變帶，在斷陷或前陸等盆地中普遍發育，其識別對闡明盆內沉積體系域，特別是構成重要油氣藏的低位域的分佈和預測具有重要意義。
  20. The main thrusts are as following : the kenxi area lies in the slope zone between the bonan depression and gudao up lift, with a mesozoic sub - strata providing a big slope background elevated in a series of steps from the bonan depression south towards the kenxi horst, and then east towards gudao uplift, and so has been affected both by the movement of the gudao uplift and the sinking of bonan depression

    通過研究認為，墾西地區位於渤南窪陷和孤島凸起之間的坡折帶，其中生界基底是由渤南窪陷向東面的孤島凸起和向南的墾西地壘逐步抬升的一個大的斜坡背景，由於孤島凸起的抬升和渤南窪陷的下降的帶動。
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