陡巖坡 的英文怎麼說

中文拼音 [dǒuyán]
陡巖坡 英文
scaur
  • : Ⅰ形容詞(山勢峻峭; 坡度大) steep; precipitous Ⅱ副詞(陡然; 突然) suddenly; abruptly
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : Ⅰ名詞(地面傾斜的地方) slope Ⅱ形容詞(傾斜) sloping; slanting
  1. The above analysis shows some results as follows : generally the discontinuities including bedding planes are favor to the stability of slope, which means that most of the slopes will not suffer large sliding failure ; most of the high slopes situated in the interest area are stable. however there are some potential unstable wedges which can be identified based on the key block theory ; some suggestions for reinforcing high slope are presented based on the stability analysis and environmental friendly consideration

    結果表明:該區邊體條件對邊整體穩定性有利;區內高以穩定及基本穩定為主,不穩定邊較少,但潛在局部不穩定塊體較多;依據邊的工程地質特徵及穩定性評價結果,對該區高的防治提出了建議。
  2. On the east terrace - fault slope of the depression, the sedimentary mode of fan - shaped delta - slump turbid fan - deep lake facies are developed. on the long axial direction of fula depression, the southeastern groove was filled with a large scale delta which was the main sources, the other little delta limited by the 3 syndepositional fault was distributed down the slope edge of the northern sub - depression. this stage developed a favorable oil sources, reservoir and regional seal which formed the good matching relations of generation, reservoir and seal in the time - space zone

    Abugarbra組的sc和sd層序發育在邊界斷層和同沉積斷層活動劇烈、湖盆擴張期,凹陷中心發育半深湖-深湖相沉積,在凹陷發育近岸水下扇,斷階緩帶發育扇三角洲?滑塌濁積扇?深湖相組合,長軸凹槽和北部次凹的北部緩帶發育三角洲體系,此層位是有利生油層和性圈閉發育層段。
  3. From sedimentology symbol such as rock assembled, sediment gradus, sandstone grading analysis, protogene sedimentary structure, ichnofossile and logging facies etc and palaeoenvironment background, it is confirmed that shen84 - an12block s34 segment is braid river delta system, not fan delta system ( abrupt slope ). then it can be more partition as braid river delta plain sedimentary assembled, delta front sedimentary assembled and prodelta sedimentary assembled on core and log assembled. and delta plain sedimentary assembled can be identified four microfacies : braided distributary channel, crevasse splay, overbank deposits and interdistributary bay

    沉積微相研究是儲層非均質性研究的基礎,研究區有豐富的芯資料和測井資料,通過石組合、沉積韻律,砂粒度分析、沉積構造、古生物遺跡和測井相等沉積學標志,結合古環境背景,確定沈84 ?安12塊s _ 3 ~ 4段為辮狀河三角洲體系,而不是前人所認為的扇三角洲(型)體系,在芯和測井組合上可進一步劃分為辮狀河三角洲平原沉積組合、三角洲前緣沉積組合和前三角洲沉積組合,其中三角洲平原沉積組合又可識別出辮狀分流河道、決口扇、分流河道邊部和分流間灣四種微相類型;三角洲前緣沉積組合識別出水下分流河道、水下分流河道邊部和分流河口壩三種微相。
  4. The study area is composed of sandstone & conglomerate reservoir of alluvial fan & fan delta, which belong to sha3 lower member and sha4 upper member of lower tertiary of yong " an town oilfield in dongying depression. the target stataum develops in the hanging wall of the synsedimentary fault in the scarp zone of dongying depression. the frequently intense movements result in the variation of sandstone and conglomerate reservoir and the evolution of the time and space of sha3 lower member and sha4 upper member in yong " an town oilfield

    研究區是東營凹陷永安鎮油田沙三下段、沙四上段的沖積扇和扇三角洲砂礫體,目的層發育在東營凹陷帶同生斷層的下降盤,因斷層多期強烈活動,導致永安鎮油田沙三下段、沙四上段的砂礫體成因類型多,時空演化變化大,在扇根一帶小層對比難度大,給油田開發帶來很大的難題,在這種背景下進行流動單元研究難度更大。
  5. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的沉積相研究發現,紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖,以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陷背景下,上升半旋迴低水位期通常發育有水下扇、湖底扇等岸近源特徵的沉積體系,下降半旋迴高水位期,扇三角洲相粗碎屑由北向南進積;在南部的凹陷緩背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。
  6. With the guidance of foundation theory such as geotechnical engineering, garden vegetation, pedology, soil magnetism and environment engineering and the base of slope ecological protection, this paper studies ecological material protection techniques which is suitable for abrupt rock slope

    本文以土工程、園林植被學、土壤學、土壤磁學、環境工程基礎理論為指導,以邊生態護理論為基礎,研究了適宜生態恢復的生態基材護方法。
  7. The main conclusions are as follows ; firstly, under the influence of three phases of episodic activities, three two - order sequences is composed of three depositional cycles and three regional unconformities ; secondly, under the control of structure activities such as fault - block activities and the influence of three - order climate cycles and source recharge, lower cretaceous can be divided into six three - order sequence ; thirdly, because fault activities is weak and fault slope is gently, fan deltas exist in steep slopes in early and later stages and subaqueous fans exist and turbidite fans exist in troughs in middle stage

    主要的結論為:其一,受三期幕式活動影響,斷陷形成了3個大的沉積旋迴和3個區域不整合面,構成了下白堊統3個二級層序;其二,受斷陷內翹傾和塊斷等構造活動的控制,以及三級氣候旋迴和物源供給因素的影響,下白堊統劃分出6個三級層序;其三,在單斷斷陷湖盆中,湖泊階段的早、晚期由於凹陷邊界斷層活動較弱,斷面較緩,可以發育扇三角洲,在湖泊階段的中期主要為水下扇砂礫體,並在窪槽區發育濁積扇。
  8. 2. rock mass structure analysis and stereographic projection are basic methods in rock slope stability analysis. this paper used these methods to analyse the stability of the fourteen slopes based close geological investigation and engineering analogy, and get some scientific conclutions

    2 、赤平投影法和體結構分析法是邊體穩定性分析的基本方法,經過詳細地質調查和工程類比,本文運用這些基本方法對沿線的14個高進行了穩定性分析,得出了較為科學的結論。
  9. The geologic condition in mountainous district is complex variable, in different geologic, it is very difficult to find the most economically design scheme. stability of 14 high - cut slopes in guangdong province is analyzed with typical rock mass structure analysis method and stereographic projection method, and with the numerical simulation method udec this paper simulated the excavation and reinforcement courses of the important slopes. some conclutions and suggestions are based the analysis above

    本文結合廣東某省道沿線14個高石邊的開挖和支護方案的選擇設計,運用常用的體結構分析方法和赤平投影方法對邊的穩定性進行了分析,採用udec數值模擬方法對一些重點邊的開挖支護進行了模擬,得出了以下一些結論: 1 、邊支護形式的選擇應遵循「安全綠色、水土保持、恢復自然、環保之路」的設計原則。
  10. According to the geological data which was gained by exploration investigation, establishing a geological model which can reflect rock mass characteristics ; with analyzing the internal and exterior factors synthetically, the deformation and possible failure mechanism and mode of the cut slopes was confirmed which combines with stereoic projection and other techniques ; the stabilities of the 14 high slopes are estimated synthetically by applicable design codes and guidelines. with the estimate result and some other analysis methods, the rock mass mechanical parameters of slope are identified ; as a results, 14 high slopes fall into 4 categories based on rockmass characteristics and discontinuities. the stability and deformation of some typical slopes was analyzed with distinct element method by udec ; the safety factor of some dangerous slopes are calculated by rigid limiting equilibrium method for comparison

    首先著重研究影響邊穩定性的內在因素,主要是通過地質勘探、測量、現場觀測等手段取得研究區地質體的基礎地質資料,建立起能夠反映地質體結構特徵的地質模型;隨后綜合分析潛在的內外部影響因素,並結合赤平投影對邊可能的失穩模式或破壞機製作出判斷;運用已有體質量分類方法對沿線14個高穩定性進行初步的評價,並結合試驗研究、經驗判斷、工程類比等手段確定了體的體力學參數;根據穩定性初步評價結果將研究區14個高按開挖方式分為4大類,並利用離散元程序udec對各類典型高進行了穩定性計算分析;對潛在危險邊利用剛體極限平衡法求出了不同工況下的安全系數。
  11. Collapses in mengshan area are caused by the weightless rock mass falling down rapidly due to the interaction of gravity and weathering factor of freeze - and - thaw action and raining action in the locate of the developing joints

    崩塌是在崖或峻的斜地帶因體節理裂隙發育,受凍融、雨水等風化作用和重力作用,造成體失穩快速下落的現象。
  12. Analysis of petroleum geology, reservoir types and distribution in lujiapu depression indicates that : the forming and distribution of reservoirs had been controlled by source area, source - reservoir relationship, petrophysical characteristics, sedimentary facies and secondary structure, and oil is most abundant in reservoirs around hydrocarbon kitchen ; the upper member of jiufutang formation which was entrained or embedded in the main oil source layer has well developed reservoir and good petrophysical property and is the principle oil - bearing interval ; the mid - fan and fan delta front of nearshore submarine fan is the most favorite facies ; the steep slope of the depression mainly consists of structural reservoirs, the slope belt mainly consists of structural - lithologic and updip pinchout reservoirs, the depressed belt mainly consists of lenticular lithologic reservoirs

    摘要對陸家堡凹陷油藏形成的石油地質條件、已知油藏類型及分佈的分析認為:生油區、生儲配置關系、儲集物性、沉積相帶和二級構造帶控制了油藏的形成和展布,其中圍繞生油窪陷的油藏含油最豐富;夾持或嵌入主要生油層中,儲層發育、儲集物性又相對較好的九佛堂組上段是主要含油層段;近岸水下扇的扇中和扇三角洲前緣是最有利的相帶:凹陷的帶以構造油藏為主,斜帶以構造性及儲層上傾尖滅油藏為主,深陷帶主要為透鏡狀性油藏。
  13. Pooling model of steep slop structure and lithological zone in north dongying sag

    東營凹陷北部構造相帶油氣成藏模式
  14. The abrupt descent of penistone crags particularly attracted her notice ; especially when the setting sun shone on it and the topmost heights, and the whole extent of landscape besides lay in shadow

    盤尼斯吞特別引起了她的注意尤其是當落日照在石上和最高峰,而其餘的整個風景都藏在陰影中的時候。
  15. Fuzzy hierarchy analysis of rock mass quality of steep sl opes of tonglushan mine

    銅錄山礦體質量的模糊層次分析
  16. Diagenesis and pore evolution of submarine fan reservoir in the west of northern steep slope, dongying sag

    東營凹陷北部帶西段水下扇儲層成作用與孔隙演化
  17. Stability analysis and deposement of high steep rock slopes of red sandstone

    紅砂質邊穩定性分析及治理
  18. In this article, idealized elastic plastic model and three - dimension finite elements programs have applied to analyzing and researching the stress and displacement distribution of 4 high - steep slopes excavated on the wan - liang expressway, and the relationship has been gained between the stress existing in excavated rock slopes and stability coefficient with depth change through the self - made fortrain program ' s application to the computation of slopes " stability coefficient ; at the same time, through the analysis of the slopes " stability coefficient, such conclusion has been gotten that cohesion in the slipping zone has important effect on slopes " stability and some proposals have been presented to improve the anti - shearing ability of the slipping body through enhancement of the cohesion in the slipping body

    本文採用概化均質的理想彈塑性模型,利用三維有限元程序分析了萬梁高速公路4個高開挖各階段的應力及應變分佈,並且編寫了fortran程序用於邊穩定系數的計算,得出邊體應力及穩定系數隨著開挖深度的變化關系。並對邊穩定系數的敏感性進行了分析,得出滑帶內聚力的變化對邊穩定性至關重要,提出了改善滑帶土粘結狀態提高抗剪能力的工程措施。
  19. However, a stability evaluation method for high and steep slope is not only concerning about general mechanics, but also about engineering geology subject and rock mass mechanics

    但是高的穩定性評價不單是個力學問題,更應該是工程地質學和體結構力學問題。
  20. Experimental study on ecological slope protection of high and steep rock slope of xiluodu hydro - power plant

    溪洛渡水電站高石邊生態護試驗研究
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