構造層 的英文怎麼說

中文拼音 [gòuzàocéng]
構造層 英文
structural layer
  • : 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...
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • 構造 : structure; construction; constructional detail; tectonic; structural; makeup; anatomy; constituti...
  1. This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement, whose tectonic deformation and magma intrusion is fiercely, and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian, it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area, such as a - granite ' s stock, batholiths and diabase ' s dike. there are many fault depressions possible

    按照不同構造層,研究了各構造層特徵:基底構造層:受早海西期作用的影響,與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓作用有關,為一變形和巖漿侵入活動強烈的古生代褶皺基底。二疊系構造層:受中海西區域性伸展斷陷作用的影響,盆地及其周緣地區發育與伸展有關的-巖漿組合,如呈巖株、巖基狀侵位的a型花崗巖以及呈巖墻狀侵位的輝綠巖等。
  2. The strata of the region are divided into two structural layers : the basement rock consisting of metamorphic rock and cover layer of mesozoic and neozoic sedimentary rock.

    將本區的地劃分為兩個構造層:既變質巖系成的基底構造層;中生代、新生代的沉積巖系成的蓋構造層
  3. Some conclusions are listed as follows : the plateform cover cap of ordos basin and its circumference areas can be divided into five tectonic sequences. the tectonic evolution of ordos basin can be classified in six stages : the basement formation phase ( from archeozoic to paleoproterozoic ) ; the aulacogen phase ( from mesoproterozoic to neoproterozoic ) ; the north china continental sea phase ( from sinian to early - paleozoic ) ; the north china intracratonic depression phase ( from late - paleozoic to early mesozoic ) ; large ordos inland basin phase and the formation of independent ordos basin ( mid - late mesozoic ) ; fault basin phase around the ordos basin ( cenozoic )

    通過研究有以下成果及認識:鄂爾多斯盆地及其周緣地區沉積蓋可劃分為五大構造層序,盆地的形成和演化分為六大階段:太古代至古元古代基底形成階段、中新元古代克拉通內裂陷槽或坳拉槽演化階段、震旦紀?早古生代華北陸表海盆演化階段、晚古生代?早中生代華北克拉通坳陷演化階段、中生代中晚期大鄂爾多斯內陸盆地演化階段及獨立鄂爾多斯盆地的形成、新生代周緣斷陷盆地演化階段。
  4. The ground stress distribution within southern margin of junggar basin assumes that its compressing stress increases vertically with depth and compatible with the structural layers , which can be divided into deep compressive belt , medium shear zone and shallow tensile fracture belt

    盆地南緣區域地應力分佈規律表現為縱向上壓應力隨深度增加而增大,並與構造層配伍,可分為深擠壓帶、中剪切帶、淺張裂帶。
  5. 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疊加的分析,對本區的應力場及變形場進行了探討,本區蓋早期階段( 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。
  6. According to the synthetically study of remnant stratum list, sediment system. character of sediment filling, comeback of archetypal basin and feature of tectonic deformation, santanghu basin passed through four formation and evolution phases : ( 1 ) formation and evolution of basin ' s basement ; ( 2 ) formation and evolution of fault - fold to depression basin in permian ; ( 3 ) formation and evolution of depression basin in triassic - jurassic - cretaceous ; (

    依據三塘湖盆地殘餘地序列、沉積體系、沉積充填特徵和原型盆地恢復,以及不同構造層變形特徵的綜合研究分析,認為三塘湖盆地經歷了如下四個發展演化階段:前二疊紀盆地基底發展演化階段;二疊紀斷陷-拗陷盆地發展演化階段; :三疊-侏羅-白堊紀拗陷盆地發展演化階段;第三-第四系新生代盆地發展演化階段。
  7. According to the type and scale of stratigraphic contact, four synthems such as basement ( pre - sinian ), lower ( palaeozoic ), middle ( mesozoic ) and upper ( cenozoic ) are divided, and seven sub - synthems are subdivided

    本文依據地接觸關系的類型和規模,將本區劃分為基巖(前震旦系) 、下(古生界) 、中(中生界) 、上(新生界)四個構造層和內部的七個
  8. The investigation in the field was combined with research indoors. by classifying tectonic sequence, confirming corresponding prototype basin, analyzing paleo - tectonic stress fields in different periods, plotting correlative tectonic map based on 297 explore wells, and analyzing the traits of the remaining depressions producing hydrocarbon and their migration rules in the ordovician, the author studied the basement of the basin ; the fault system of the basin ; the tectonic - sedimentary evolution of the basin and its circumference areas ; the prototype basin and corresponding dynamics background ; the paleo - tectonic patte rn and its evolution in the layers of producing gas in different periods of ordovician ; the superposition relationship among the different period basins formed by different stress fields ; the reformation of the basin and the formation, redistribution and final emplacement of the gas pools

    採用野外地質調查與室內綜合研究相結合,通過構造層序的劃分及其相應盆地原型的確定、不同期次古應力場的分析、以297口探井數據為基礎的相關圖件的編制、奧陶系殘餘生烴坳陷及其遷移規律研究等的綜合分析,開展了盆地基底以及盆地斷裂系統、盆地及鄰區與沉積演化、盆地原型及其形成的動力學背景、奧陶系產氣不同時期的古格局及其演化、不同期次應力場形成的不同世代盆地之間的疊置關系以及盆地改與天然氣藏的形成、重新分配和最終就位諸方面的研究。
  9. The velocity difference between the two layers of the lower crust is not obvious

    下地殼的兩構造層速度差異不明顯。
  10. Classification of tectonic sequence and dynamic evolution of jixi basin, eastern heilongjiang province

    黑龍江東部雞西盆地構造層序劃分與盆地動力學演化
  11. Stratum composition in xiaoqinling represents early precambrian crystal basement and mesoproterozoic era cover rocks of the typical north china craton

    小秦嶺區內地具有典型華北型早前寒武結晶基底和中元古代以來的蓋,不發育晚古生代、中生代構造層
  12. Through studying the stratigraphic framework of tectonic sequence, the characteristics of deposits and multi - episode tectonic movements show the eastern qinling and dabie orogenic movement and basin formation processes

    晚白堊世至古近紀區域背景發生重大變化,構造層序記錄了晚燕山期地殼快速均衡隆升,伸展斷陷盆地形成演化過程。
  13. Different tectonic style exists in the upper and lower layers of the yanshanian boundary. the lower layers takes on the tectonic style of thrust fault and nappel. the upper layers hi step positive fault

    2 、盆地燕山期界面上下不同構造層具有完全不同的樣式,界面下伏構造層呈現沖斷褶皺、推覆樣式,界面上覆樣式為階梯狀正斷,整體呈現「雙」結型式。
  14. You can argue that the most compelling applications for p2p have yet to be invented, and if jxta ended up with policy - or implementation - specific details embedded into its fundamental infrastructure layer, such undreamt - of applications might never work with the platform

    您可以爭辯說, p2p最引人注目的應用程序尚未開發,那麼如果jxta把特定於策略或實現的細節嵌入其基礎構造層后就完事的話,那麼這些尚未想像到的應用程序就可能永遠不會和這個平臺一起工作。
  15. Multistage structural deformations are experienced in kongquehe area, the basical fault systems of nww - near ew, nne - near sn, nnw and nee are established, the fault movement has the characteristics of multistage and inheritance, in the area multi - structural deformations are experienced in sinian to early ordovician, early ordovician - silurian, jurassic cretaceous - caenozoic, etc. late structural deformation shapes are changed for different levels of formar structural layer, in which different deforming shapes are created and integrated overlying of deformation is induced

    摘要孔雀河地區經歷了多期次的變形作用,形成了現今北西西近東西向、北北東近南北向、北北西向和北東東向基本斷裂體系,同時斷裂活動表現為多期性和繼承性的特點;該區經歷了震旦紀至早奧陶世、早奧陶世末志留紀、侏羅系、白堊紀新生代等多期變形作用,且後期的變形作用在不同程度上對前期的構造層的變形樣式有所改,形成了有一定差異的變形面貌,成變形的復合登加。
  16. Note that we also cache all of the results. this is used for cycle detection and for building hierarchies later

    注意,我們還緩存了所有結果,這用於循環檢測和在以後構造層次結
  17. If you make your top - level exception too specific you ll end up having to restructure your hierarchy later to fit in something more generic

    如果您將頂級異常搞得太具體,那麼其結果是您今後將不得不重新構造層次結,以適應某些較通用的情況。
  18. The dislocation interfaces, which have different directions, different combinations, different scale, different deformation strength and different properties, are belonged to shallow structure. they are the products of multi - stages, multi - periods and multi - causes of movement during the himalayan epoch. they were controlled by and resulted from 2 structural stress fields of ne structure and nw structure

    由此認識到,壩區發育的不同方向、不同形態和組合型式、不同規模、不同變形強度和不同性質的錯動帶屬于地殼淺部構造層次,是本區喜馬拉雅運動多期次、多階段、多成因的產物,分屬于區域上ne向帶和nw向帶的成分,並受控于這兩期應力場。
  19. Comprising 50249 density data, 11374 magnetic susceptibility data and 8889 remanent magnetization data, the regional stratigraphic physical column column based on stratigraphic regionalization has been set up to guide geophysical survey in jiangxi province, southern china

    摘要對巖礦石50249個密度、 11374個磁化率、 8889個剩磁強度數據,以江西省及其地區、地分區為研究區,以構造層、年代地為單元進行區域地物性的統計,結果為該區的區域物探、礦區物探工作提供基礎。
  20. The basin has three evolutionary stages including intracontinental rift basin in p1 - p2, down basin in t2 + 3 - k and the strong trust - orogeny process in n - q. according to the unconformity contact relationship and sedimentary components, santanghu basin is divided into four tectonic sequence such as : o - c tectonic sequence of basement, pi - p3 tectonic sequence, t - k tectonic sequence and n - q tectonic sequence

    根據盆地地之間的不整合接觸關系,考慮到各序沉積物組成與生物組合特徵等因素,將三塘湖盆地劃分為: ( o ? c )基底構造層序,二疊系( p )構造層序,三疊系( t ) ?白堊系( k )構造層序和第三系、第四系構造層序。
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