斷階帶 的英文怎麼說

中文拼音 [duànjiēdài]
斷階帶 英文
step-fault zone
  • 斷 : 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...
  • 階 : 名詞1. （臺階） steps; stairs 2. （等級） rank 3. [醫學] （耳蝸的三個螺旋管的任一個） scala 4. [數學] order 5. [地質學] stage
  1. The dimensions of rupture zones in various island areas appear to be related to the extent of prominent deep-sea benches.

    各種島嶼內斷裂帶的大小似乎與突出的深海階地的范圍有關。
  2. Discontinuous oblique derivative problems for second order mixed equations with parabolic degeneracy

    帶拋物退化線的二階混合型方程的間斷斜微商
  3. 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，在凹陷陡坡發育近岸水下扇，斷階緩坡帶發育扇三角洲?滑塌濁積扇?深湖相組合，長軸凹槽和北部次凹的北部緩坡帶發育三角洲體系，此層位是有利生油層和巖性圈閉發育層段。
  4. Having analyzed preliminarily formation mechanism of these common characteristics of anomaly, it concludes that : these are results, controlled by basically united tectonic stress field of large - range, caused by stress - strain accumulation and certain phase strong earthquakes, according to deformation difference brought about in tectonic position along the boundary zone and within second - order faults of active blocks resulted from unstable and inharmonious features for movement of block system at different levels and deformation of boundary

    分析這些異常共性特徵的形成機制，初步認為：是在基本統一的大區域構造應力場控制下，不同層次塊體系統運動及其邊界帶變形的非平穩、非協調性，在活動地塊邊界地帶和地塊內部次級斷裂構造部位產生變形差異而導致應力-應變積累、孕育強震到一定階段的結果。
  5. The existence of silent earthquakes gives scientists a completely new angle on the slip process by permitting the detailed study of fault zones through every stage of their movement

    然而，無聲地震的存在卻提供科學家一個全新的角度，來看待斷層滑動的過程，讓他們對斷層帶運動的每個階段做更仔細的研究。
  6. Along with the global broad band industry chain formation development as well as the dsl technology unceasing expansion, iptv spring already arrived, has entered one rapid growth stage

    隨著全球寬帶產業鏈的形成發展以及dsl技術的不斷擴大， iptv的春天已經來到，並進入一個飛速增長階段。
  7. The conclusions are : under the case of monopoly, the enterprise has the ability to delay the investment, thus it can take the advantages of option value brought by uncertainty to select the optimal timing of investment in each phrase flexibly ; under the case of competition, enterprise will select the optimal investment timing by comparing the tradeoff between the benefits of option value and the strategic lost of competitor ' s preemption, because preemption of competitor will reduce the ability of enterprise to delay investment comparing with the case of monopoly, the enterprise usually invests early, hi the meantime, by comparing the outcomes of investment cooperation in the r & d phrase with that of competition, we can conclude that r & d investment cooperation is pareto dominant strategy, since enterprise can fully take advantage of the option value brought by uncertainty, and thus enhance the flexibility of decision - making

    得到的結論是：在壟斷情形下，企業具有延遲投資的能力，因而企業可以充分利用不確定性帶來的期權價值，在創新投資的各階段根據不確定性信息的獲得靈活地選擇最優的投資時機；在競爭情形下，企業延遲投資的能力受到局限，由於害怕競爭對手的佔先，企業為了獲得佔先效應，會考慮競爭對手的行為對自己的影響，通過在不確定性所帶來的期權價值與競爭對手的行為所帶來的戰略價值之間進行權衡，來選武漢理工大學博士學位論文擇最優的投資時機。與壟斷情形相比，一般企業會提早投資。同時通過分析說明，競爭企業間通過在創新投資的研究與開發階段進行合作，可以使兩家企業充分利用不確定性帶來的期權價值，增強決策的柔性，結論說明，合作創新投資是兩家企業的帕累托占優策略。
  8. With the enhanced exploration and development of oilfield, in order to find more favorable hydrocarbon accumulation zone, or increase productivity, facies analysis is needed. log data is an important means in facies analysis

    隨著油田勘探開發程度的不斷提高，要找到有利的油氣聚集帶和開發階段提高採收率，都必須進行儲層沉積相分析。
  9. The high, middle and low people of every stratum of both sides say for entering a war, it is an cruel, unwise, wrong, error in judgement, the racial discrimination one, war fierce and brutal and with prejudice

    對于參戰雙方的高中低各階層人民來說，它都是一場殘酷的愚蠢的錯誤的判斷失誤的種族歧視的帶有偏見的和兇暴的戰爭。
  10. According to the analysis of the structure deformation variant direction the structure superposition during late period, and the tectonic stress field and deformation variant field, the cover extended nearly sn direction in early stage ( d - c ), maybe changed the direction in pernian ( especial the late permian ), and developed some new half - graben along sn direction except the succession activity at great fault zone. the direction of compression deformation variant, however, was nearly sn direction in indo - chinese epoch, ne - sw direction in early yanshan movement epoch, nne - ssw direction in late yanshan movement epoch, and transformed from ew to sn direction in himalayan movement epoch

    根據不同構造層中變形方向及後期構造疊加的分析，對本區的構造應力場及變形場進行了探討，本區蓋層早期階段（ d - c ）為近南北向的伸展拉張，二疊紀（特別是晚二疊世）的伸展方向可能發生了改變，除在各斷裂帶繼承性活動外，沿南北方向又新生了一些半地塹。而在擠壓變形時，印支期主要為近南北向擠壓，燕山早期為nw - se向擠壓，燕山晚期為nne - ssw向擠壓，而喜山運動可能經歷了從ew向向sn向方向擠壓的轉變。
  11. We predicated three favorable zones : the excellent play is at the downside of the east terrace - fault slope, the good play is distributed on the depression ' s steep, the common play around the edge of the slope of the depression

    發育扇三角洲砂體的東部斷階斜坡帶中下部、發育三角洲砂體的東南凹槽和東北部緩坡帶是最有利的目標區，發育近岸水下扇的西部陡岸帶是較有利區帶，緩坡帶的上部邊緣為一般勘探區。
  12. Multi - stage strike - slip motion and uplift along the altyn tagh fault since the late cretaceous

    晚白堊世以來沿阿爾金斷裂帶的階段性走滑隆升
  13. 7. it is indicated the prospects for exploration are beidagang bueried - hill - drape - lik fold oil accumulation belt, baidong structure belt and chengbei fault step oil accumulation belt, which directs the explorations of neogene in qikou depression

    7 、指出了有利的勘探區帶是北大港潛山?披覆背斜油氣聚集帶、白東構造帶和埕北斷階式油氣聚集帶，為歧口凹陷上第三系的勘探明確了實施方向。
  14. Zijingguan fault zone is the main structure in taihang mountains that are located in the central part of 20 ~ 30 ne - striking daxing ' anling - taihan - wuling tectonic belt. it is composed of two diagonalized faults that are wulonggou - shanghuangqi fault located in the west and zijingguan - lishan fault in the east

    紫荊關斷裂帶是大興安嶺?太行山?武陵山構造帶中段太行山地區的主體構造，總體走向20 30 ，由西側的烏龍溝?上黃旗斷裂和東側的紫荊關?靈山斷裂左階斜列組成。
  15. Several normal faults within the hainan fault zone constitute a fault - step zone and form a narrow and steep zone, which controlled the development and distribution of depositional systems in this area

    研究認為，海南斷裂帶的幾個北掉斷層構成斷階帶，形成湖盆邊緣陡且窄的地貌特點，控制了該區沉積體系的展布規律。
  16. Optical stimulated luminescence dating of late pleistocene terrace deposits in the eastern segment of the altyn tagh fault and its tectonic implication

    阿爾金斷裂帶東段晚更新世階地沉積物紅外釋光測年及其構造意義
  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. Gubei slope locates in the middle structure area of bohaiwan basin which stretch toward near north and south, and the faults which tend towards east and west spread all over of the whole district. three huge faulty trap whic h control the sediment formation growth distribute in order, which result in the stratigraphy dropping in step along the slope

    孤北斜坡帶地處于渤海灣盆地中部近南北向伸展的構造區上，近東西走向的斷層及其斷裂帶縱橫全區，三階大斷裂沿斜坡規律性分佈，基本上控制了全區地層的發育，使得地層沿斜坡坡降式分佈。
  19. First, it can be seen through market environmental analysis that with the fast growth of chongqing economy, the increase of mid class, the new developing opportunities for chongqing ping an life insurance company with the entry of wto and the lower competitive intensity of chongqing life insurance market of under oligopoly, the coming 3 - 5years will become a chance window of development of chongqing ping an life insurance company

    首先，通過對營銷環境的研究可以看出，重慶經濟的高速成長、中產階層的不斷擴大、加入wto將帶給較早市場化、國際化的重慶平安的新的發展機遇和目前仍處于競爭強度不高的寡頭壟斷階段的重慶壽險市場等等，都預示著未來3 ? 5年將是重慶平安人壽發展的「機會窗」 。
  20. Qinglong fault zone evolved successively by phases in a long term : it probably formed in the late period of paleoproterozoic and rejuvenated in a large scale during jurassic and cretaceous

    青龍斷裂帶形成時間早，演化過程具長期性、階段性和繼承性特點，斷裂帶可能形成於早元古代末期，侏羅紀?白堊紀時，斷裂帶大規模復活，右行走滑作用為主要活動機制。
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