弱震區 的英文怎麼說

中文拼音 [ruòzhènqū]
弱震區 英文
weak earthquake zone
  • 弱 : Ⅰ形容詞1 （氣力小; 勢力差） weak; feeble 2 （年幼） young 3 （差; 不如） inferior 4 （接在分數或...
  • 震 : Ⅰ動詞1 （震動） quake; shake; shock; vibrate 2 （情緒過分激動） be greatly excited; be deeply ast...
  • 區 : 區名詞（姓氏） a surname
  1. With practical engineering examples, this paper deals with the collection of surface wave signal along with seismic refraction exploration, the utilization of surface wave components to make analysis during data processing, the thickness division of overburden bed, strongly - weathered bed, intermediately - weathered bed and weakly - weathered bed in combination with the refraction data, and mutual reflection and interpretation of the burial condition of the bedrock surface

    筆者結合工程實例，介紹了在地震折射勘探中同時採集面波信號，在資料處理時利用面波組份進行分析，配合折射資料對測區覆蓋層、強風化層、中風化層及弱風化層厚度進行劃分，同時相互映證解釋基巖面的埋藏情況。
  2. Guided with the theories of plate tectonics and complex hydrocarbon system, based on the analysis of geological factors of hydrocarbon pools in the northern area of tarim basin, the author puts forward the geological background favorable for and the possible areas most suitable for the formation of complex traps. the identification and description of complex traps lead to the recognization of five large and four middle or small complex traps, by the means of the main techniques and methods include the detailed interpretation of seismic profiles, drilling, logging, map compiling based on the depth of sealing surface and on the superimposed relation of stratigraphic lithology over and beneath the unconformity surfaces, and the the use of the reversion of jason and 3d coherent data. at the same time, the major controlling factors of complex trap oil pool have been analyzed based on the case study of typical oil pools in the paper

    目前，復合圈閉勘探及研究工作在我國還比較薄弱，本文以板塊構造學、復式含油氣系統等理論為指導，通過對塔北地區石油地質特徵的整體解剖，從動態的角度，綜合分析和探索了塔北地區復合圈閉形成的地質背景及發育的有利區帶和領域，根據鉆、測井及地震剖面精細解釋成果，採用封閉面編圖、不整合面頂底板地層巖性疊置關系編圖方法和jason及三維相干數據體等地球物理反演技術，發現大型復合圈閉顯示2個，中小型復合圈閉4個，復查落實大型復合圈閉3個，並通過典型油氣藏解剖，分析了塔北地區復合圈閉成藏主控因素分析。
  3. Since 1980, there are many countries and regions who have experienced serious banking problem in the world. the weakness of bank and bank crisis are become the economic p roblem of the world. the east - south asia financial crisis make the world astonished

    自1980年以來，全世界有130多個國家和地區在不同階段經歷了銀行業的嚴重問題，銀行的脆弱性和銀行業危機已成為全球化的經濟問題，特別是1997年的東南亞金融危機震驚了世界。
  4. It divided the south china magnetic fields on the basis of intensities of analytical signals and, in combination with the achievements in seismic and isotopic geochemical studies of south china granites, investigated the deep geological backgrounds for the division of magnetic fields

    根據解析信號的強弱，對華南磁場進行了分區，並結合地震和華南花崗巖同位素地球化學的研究成果探討了磁場分區的深部地質背景。
  5. At the same time watertight rock surround the carbonate rock, which is helpful to water percolate deeply and trigger earthquake

    同時，峽谷區碳酸鹽類巖石周圍又有弱透水和微透水的巖層包圍著，有利於庫水向深部滲透，誘發地震。
  6. As one content of the layout of earthquake - resistent and damage prevention of zhongzhou city, researches in damage prediction and correspond strategies of buildings have been carried through in two aspects as following : firstly, the domestic and aboard methods of damage prediction of buildings are compared and studied. the general methods, corresponding advantages and disadvantages as well as the scope of application for earthquake damage predicting of buildings are summarized. the main problems and solutions for earthquake damage predicting of buildings are submitted ; secondly, the current situations of buildings in the urban areas of zhangzhou city have been investigated

    作為漳州市抗震防災規劃的內容之一，本文就建築物震害預測及防禦對策著重開展了兩方面的研究工作：一是對國內外建築物震害預測方法的分析對比，總結了建築物震害預測的一般方法、優缺點及其適用范圍，並提出了目前建築物震害預測存在的主要問題及解決措施；二是開展了漳州市區建築物現狀調查，闡述了漳州市區主要建築類型的震害預測方法和步驟，給出了震害預測的計算實例，完成了漳州市區建築物震害預測、地震經濟損失、無家可歸和傷亡人員的估計，指出漳州市區建築物抗震防災的薄弱環節，並提出了相應的防禦對策。
  7. Aimed at the present code of structure design without the specific method of frail - layer check computations of frame structures in high vibration areas, this article provides the parameter modifying method for the checking according to different regulations of earthquake parameter and by deducing and contrasting the relation of elasticity and plasticity displacement angle limitation of several earthquakes from the given conditions of present code

    摘要針對現行結構設計規范中沒有明確給出高震區框架結構薄弱層驗算具體方法的情況，從規范給定的條件入手，通過時大、小地震下彈性、彈塑性位移角限值關系的推導和對比，提出了在高震區框架結構薄弱層驗算中進行參數修正的方法。
  8. Because the yilan - yitong fault belt has blocked and weaken the effect from the pacific plate diving, it was difficult for the energy to accumulate to induce earthquakes on a large scale in the basin

    盆地東側的依蘭-伊通斷裂帶（郯廬斷裂帶北段的一部分）阻擋和削弱了太平洋板塊向西俯沖對其地區的作用。能量難以在盆地內積累很大而引發大規模地震。
  9. We can determine ineffective water supplying area and the rate of water supply of node by analysing the reliability of system with monte carlo method, find the weak link, and provide technique and countermeasure for damage prediction and aseismic reinforcement. finally, the estimate method of losing is developed for water delivery system under earthquake

    通過用montecarlo技術對管網的連通性分析，確定節點的供水率和系統供水失效區，找出系統的薄弱環節，這可以為城市供水管網的震害預測和抗震加固提供有效的方法和對策。
  10. The paper also carried out elastic and plastic analysis on 8 - storeyed truss and 8 - storeyed vierendeel truss. based on the results, the two structures can both be applied to strong earthquake zone. however, the weak layer of the former structure is the first storey, while the weak layer of the latter is the 3rd storey

    本文還對8層的混合式鋼結構交錯桁架體系、 8層的空腹式交錯桁架體系的進行了彈性和彈塑性分析，從分析結果中可以看出， 8層的兩種形式的結構都適合用於8度強震區的三類場地土區，但混合式的薄弱層是在結構底層，而空腹式的薄弱層是在結構的第3層，而且兩者的破壞模式也有所不同。
  11. The disturbance located at inner region and near eyewall intensifying corresponds to the growth of amplitude of typhoon maximum tangential velocity with shorter period and the opposite is true. the weakening role of periphery disturbance intensity drop in typhoon maximum tangential wind reduces iv rossby obviously and the mean tangential wind display a strong vibrational characteristic for the periphery disturbance intensity growth

    臺風內核區和眼壁附近擾動的減弱（加強）使臺風最大切向風速的增幅減小（增大） ，且強度增強，風速變化的震蕩性加強，震蕩的周期縮短；強度減弱，風速變化的震蕩性減弱，震蕩的周期加長。
  12. The most distinct intensification in maximum azimuthally mean tangential velocity occurs when the convective patch is positioned in rmw, the second in the interior region. this intensification exhibit distinct vibration with 6 ~ 7h period and the vibration in inner region diminishes with shorter period

    Rmw附近擾動使最大平均切向風速增大最明顯，其次是內核區，而且這種增強表現出顯著的震蕩特徵，震蕩周期約為6 7h ，內核區的震蕩較弱，震蕩周期略短。
  13. The main conclusions are as follows. cross - fault displacement observation can directly reflect the recent activities of the major faults in the region. present fault movement and earthquake activity have a temporal correspondence with each other, they all show alternately quiet and active periods. the intensity of fault movement is a manifestation of the strength of regional principal compressional stress, it also indicates the strength of an earthquake in preparation

    認為： 1 ）跨斷層位移觀測資料能夠直接反映區內主要斷層的最新活動情況； 2 ）斷層現今活動與地震活動在時間序列上相互對應，均有活躍期與平靜期相互交替出現的活動特徵； 3 ）斷層活動強弱是區域主壓應力強弱的表現，亦是孕震強度的標志。
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