構造形跡 的英文怎麼說

中文拼音 [gòuzàoxíng]
構造形跡 英文
structural feature
  • : Ⅰ動詞1 (構造; 組合) construct; form; compose 2 (結成) fabricate; make up 3 (建造; 架屋) bui...
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • : 名詞1 (留下的印子; 痕跡) mark; trace 2 (前人遺留的建築或器物等) remains; ruins; vestige 3 (...
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  1. We can avouch that the future typical organization structure of enterprise should be opening network, which is fit for the requirements of information revolution and digit - and netization this article is intended to describe clearly the historical background, developing train and future trend of the enterprise organization structure ' s evolution, explain the general theory on the design of organization structure and make further analysis of several representative organization structures, especially of the reconstruction of the business procedures

    本文力圖清晰描繪企業組織結變遷的歷史背景、軌和未來趨勢,對組織結設計的一般原理進行了闡述,對具有代表性的幾種組織結進行了較深入的剖析,尤其對業務流程再組織進行了深入的探討,文中最後以海爾集團組織結的變革為例再次說明了隨著企業的成長,企業的組織結是在不斷變革的,尋找適合自身企業發展的組織結式至關重要。
  2. Sliding structures are recognized appling multiple ways, and they occur in sections in the shape of flowers. the main sliding fault has the characteristics of straightness and sectionality in plane view. in the main displacement belt or its adjacent areas, an echelon faults and an echelon folds appeared

    應用多種標志識別走滑,主要表現為剖面上出現花狀,主走滑斷層平面上呈平直狀和分段性,在主位移帶內或其毗鄰地區出現雁列斷層及雁列褶皺,在主幹斷裂帶兩側的褶皺可見火山巖體被錯開,位移2 4km ,在鉆井巖心樣品中見到明顯的走滑運動
  3. For better understanding the influence of tectonic structural features in soil mass to subgrade of infrastructure, the author defined the faults, structural joints and structural fissures as neogene tectonic structural planes, and studied the features of the planes with the methods of systematic analysis

    摘要為闡明土體中存在的構造形跡對工程建()築物地基的影響,將土體中的斷層、節理和裂縫統稱為土體新近紀面,用系統分析方法對土體新近紀面特性進行了分析。
  4. The results show that the planes are widely distributed and lie concealed, being the deformation traces left over by the seismological fault in the soil mass and in direct response to the recent tectonic activities, whice greatly influences on the stability of the soil mass as a part of the infrastructural subgrade

    結果表明:土體面分佈廣泛且具隱伏性,是發震斷裂在土體中留下的變,是近期活動最直接的反映,對工程地基土體的穩定性有重要影響。
  5. Being affected by “ continent drifting theory ”, “ plate structure theory ”, etc. people has long paid particular attention to internal force while ignored external force ? such as meteorite strike event

    該影響最顯著的標志是,它使地球表面廣泛分佈了大規模的隕擊遺? ?環山系,斜巖是該類山體最普遍的巖層紋理
  6. According to the movement traces of yarn carriers on the braiding machine bed, a perform was divided into three regions, i. e. interior, surface and corner, and distinct control volumes were defined for each region. analyzing the control volume of each region, the yarn architecture of perform was described and three kinds of local unit cell were identified. then the relations between the braiding parameters of the perform were derived

    根據編織過程中攜紗器的運動軌特點,將預成件劃分為三個不同的區域,分別定義了不同的控制體積單元,識別了預成件的兩種局部單胞模型,分析了預成件的紗線,並導出了編織結參數之間的關系,同時給出三維編織復合材料的設計方法。
  7. The present thrust nappe structure formed in late jurassic according to comprehensive analysis of sedimentary, structure and fission track tesing result

    據沉積、和裂變徑測試結果綜合分析認為,現今所見的賀蘭山逆沖推覆成於晚侏羅世。
  8. Discontinuities or weakness planes are those structural features which separate intact rock blocks within a rock mass.

    不連續面或弱面指在巖體內分割完整巖石的那些構造形跡
  9. The variation of regional stress field can be genetically interpreted by the rotation speed variation of the earth and its impact on the movement of lithosphere plate and deep processes of the earth, it is also related to the earlier structural feature and boundary of the basin

    區域應力場變化可以用地球自轉速度變化引起的巖石圈板塊活動及觸發的深部過程來解釋,亦與先期構造形跡和盆地邊界條件有關。
  10. Depending on how the ground surface is denuded, the feature of the current crustal stress field and rock stress environment can be calculated analyzing the result in this paper : by analyzing the recovering feature of the elastic deformation of the rockmass in unload - stage under various pressures, it has been found there is close relationship between the recovering degree of the elastic deformation of the rockmass and the unloading degree of the pressure the direction of the major principal stress in the crustal stress field is not consistent with the direction of the crushing stress regional tectonics borne during the last tectonic movement. the evolving degree of the regional geomorphology evidently affects the current crustal stress field, which changes from the self - weight stress field to the horizontal stress field, with the changing of the eroding degree of the regional geomorphology ranging from valley area to hilly country to flat country. in valley area, where there is two stress belts, the bankslope s tress belt and the self - weight stress belt within the mountain. the direction of the major principal stress is nearly parallel to the ground surface and inclines towards the valley in the bankslope stress belt. it is nearly vertical in the self - weight stress belt

    通過本文的研究成果,根據區域性地貌的演化特徵,我們可以大致地對現今地應力場進行判斷:在分級卸荷條件下,巖體中彈性變的恢復具有明顯的規律性,這種規律對于研究地應力場的演變是有幫助的;地應力場中最大主應力方向與區域構造形跡在最近的運動中所受區域性擠壓應力的方向無明顯的對應性;區域性地貌態的演化程度對現今地應力場的特徵具明顯的影響,隨著區域性地貌侵蝕程度由峽谷區、丘陵區、平原區的變化,現今地應力場特徵由自重應力場、水平應力場為主含少量自重應力場特徵向水平應力場的規律變化;在峽谷區,山體中具有兩個應力帶:自重應力帶和卸荷應力帶,最大主應力方向在卸荷應力帶中近平行於坡面並傾向于河谷、在自重應力帶中近於直立;根據原始地面遭剝蝕的程度,可以大致地估算最大主應力和中間主應力的量值和方向;在丘陵區和平原區,最大主應力的方向近於水平,並與附近區域性侵蝕盆地和河流的展布方向基本平行,根據原始地面遭剝蝕的程度,可以大致估算其最大主應力的量值;根據區域性地貌態的特徵來分析工程區的現今地應力場特徵,並進而大致了解巖石的應力環境,這種分析方法得出的結論與許多實際的地應力測試成果基本一致,對于大型水電工程地下廠房和壓力隧洞的設計是有所幫助的。
  11. The analysis of structural movement and expression shows that qinqi tectonic active area is a volcano - sendimentary compressional depression formed by several times of compression movement from lower proterozoic, and spreaded in the direction of north step by step till the forming of xiangshan and miboshan group in mid - later period of ordovician, bearing hardly with volcanical rock

    從秦祁活動帶的構造形跡分析認為,該帶是自下元古以來多期擠壓環境下成的火山一沉積壓陷,並一期又一期向北蠶食,于奧陶紀中後期成基本不含火山巖的米缽山組、香山群壓陷巖系。
  12. It introduces the appearance of layer slide structure in coal mine production and analyzes the character and application in mine geology work

    介紹了層滑在煤礦生產中的表現,分析了層滑的特徵及其在礦井地質工作中的應用。
  13. Abstract : it introduces the appearance of layer slide structure in coal mine production and analyzes the character and application in mine geology work

    文摘:介紹了層滑在煤礦生產中的表現,分析了層滑的特徵及其在礦井地質工作中的應用。
  14. With the scale extending, the enterprise organization has changed from orderliness to chaos in the evolution process. so it is important for the sustainable development of enterprise to lead in organizational innovation which can make enterprise to create effective energy, absorb the negative entropy, reduce positive entropy and accelerate the formation of managerial dissipative structure

    企業組織在發展過程中隨著規模的擴大,其軌呈現出從有序到無序的內在演變過程,因而通過組織創新引導企業不斷創有效能、吸收負熵流、減少正熵流、促進管理耗散結成,對推動企業可持續發展尤為重要。
  15. So, it provides many new ponderations and enlightenments in understanding holocene stratum and basement tectonics of the hebei plain

    因此,它對全面認識河北平原的全新世地層和新運動會有許多新的啟示。
  16. What the practical problems is often gotten is a single variable time series which has a time interval of t, reflect by a lot of interactive physics factor, containing the mark of all variates participating in movement, traditional time series analysis is to analyse going from this array to the form directly it ' s time develops, one dimension analysis loses useful information, the characteristics of phase space reconstruction method is to construct one dimension scalar quantity to high dimension vector, prop the geometry space of the state, show all dynamical information of system in phase space. the characteristic that just constructs again according to the phase space in this text, analyse the time series of responding, use the relevant knowledge of symbol dynamics and reconstruct phase space, put forward a kind of relation degree analysis method of the systematic mathematics model which has theory basis, so reach the correction of calculation mathematics model, make it accord with the actual systematic state

    實際問題中常常得到的是一個時間間隔為t的單變量的時間序列,它是許多物理因子相互作用的綜合反映,蘊藏著參與運動的全部變量的痕,傳統的時序分析是直接從這個序列去式地分析它的時間演變,一維分析必然喪失許多有用信息,相空間重方法的特點是把一維標量數據成高維矢量,支起狀態的幾何空間,在相空間中展示系統全部動力信息。本文正是根據相空間重的特點,對響應時間序列進行分析,利用符號動力學、重相空間等方法,提出一種有理論依據的系統數學模型關聯度分析方法,從而達到修正計算數學模型,使其更符合實際系統狀態的目的。
  17. This method can be briefly summarized as follows : based on the reconstruction of the process of formation of related ore deposits and construction of metallogenic models, reconstruct some important ore - forming geological events and their evolution processes are reconstructed by tracing the tectono - deformation petrofacies in the ore sources series, study the distribution patterns of ore materials in a series of geological events and indicators and degrees of gradual ore material concentration and formation of ore deposits and further explore and direct evaluation of regional resource potentials, mapping and mineral exploration in ore deposit concentration areas

    成礦地質事件評價方法,就是在恢復礦床成過程並建立成礦模式的基礎上,通過對礦源巖系的巖相追索來恢復與成礦有重要意義的地質事件及其演化過程,研究在這一系列地質事件中成礦物質的分佈規律和逐步富集成礦的標志及程度,並用以進一步探索、指導區域資源潛力評價和填圖找礦的方法。
  18. By using the method of construct boundary condition at the entrance, it did a research on the formation principle of karman vortex and believed that there was no direct relationship between the formation and the object itself. the existence of the object just provided a basic current in the space to generate a absolutely unstable district and so the explanation of absolutely unstable model near wake flow is more suitable

    通過採用入口邊界條件的方法,對k rm n渦街的成機理進行研究,認為渦街的生成與物體本身無直接關系,物體的存在只是在空間內提供了可以產生絕對不穩定區域的基本流,因而近尾絕對不穩定模式的解釋較為合適。
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