推覆體 的英文怎麼說

中文拼音 [tuī]
推覆體 英文
decken
  • : 動詞1 (向外用力使物體移動) push; shove 2 (磨或碾) turn a mill or grindstone; grind 3 (剪或削...
  • : 動詞1. [書面語] (蓋住) cover 2. [書面語] (底朝上翻過來; 歪倒) overturn; upset 3. 同 「復」 (Ⅱ1. 2. )
  • : 體構詞成分。
  1. Cenozoic deformation and propagation of the kalpintag fold nappe

    柯坪塔格推覆體的新生代變形與擴展
  2. ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper. the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting, which is of great theory significance for studying regional structural framwork, relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin. moreover, the result is of guidance significance for the forecast of combination gas, distributing and formation of nappe metal deposit in northern qaidam basin

    ( 6 )論文探討了賽什騰? ?錫鐵山斜向逆沖構造的地質意義,認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應的結果,該認識對于研究柴北緣區域構造格局、盆山關系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義,對柴達木北緣的油氣預測、推覆體金屬礦床的分佈、形成具有指導意義。
  3. This paper has studied the development of setting & model of the overthrust, which is distributed over the plane & section, and its belting character in the northern margin region of chaidamu basin, and described the character of the main overthrust sheet belt and lower strain area in great details. moreover, it has pointed out a best target for oil / gas exploration on the imbricate fan belt and hidden overthrust forward belt through surveying the developing evolution model and its formation mechanism of the overthrust in the field and structure inversion indoor 6figs., 8refs

    研究了柴北緣地區逆沖構造的發育背景、發育模式,平面、剖面展布特徵及其分帶性,並對主幹逆沖斷裂帶及其間的推覆體帶、逆沖席帶和低應變區的特徵進行了詳細描述,同時通過野外觀察和室內構造反演來研究構造的發展演變模式及其形成機理,指出其逆沖疊瓦扇帶和隱伏逆沖前緣帶是最有利的油氣勘探目標.圖6 ,參8
  4. All the pre-shamvaian rocks in the selukwe area lie on the inverted limb of this fold.

    塞盧奎地區的所有前沙姆凡巖石均分佈於此推覆體的倒轉翼中。
  5. To do the investigating and studying work about the achievements of tackling key problem of the quondam exploration of front - zone of mountain, to analyze and study the applicability about the gathering technology used in the seismic exploration of the complicated construction belt of front - zone of mountainous ; 2. combining the quondam achievements, researching the design method of observation system objective of the complicated construction belt based on seismic - geology model, firstly, building the surface level and deep layer seismic - geology model of complicated construction belt and analyzing the forward model, secondly, designing the observation system aiming at the overthrust nappe structure in section and in area ; 3. aiming at the complicated earth ' s surface condition of front - zone of mountain, how to select the exciting method and the parameter, how to optimize the environment of exciting method and reception, how to pledge the normal combination of the datum of different exciting method ; 4

    根據山前帶的地震地質條件特點,本文主要研究了以下幾個方面的內容: 1 、對以往山前帶地震攻關成果開展調研工作,分析研究在山地山前復雜構造帶所採用的地震勘探採集技術的適用性; 2 、研究基於地震地質模型的復雜構造帶觀測系統目標設計方法:如何建立復雜構造帶的表層、深層地震地質模型,利用正演分析目標區的觀測系統;針對逆掩推覆體構造,如何分區分段有針對性設計觀測系統等; 3 、針對復雜地表條件的山地山前帶,如何選擇激發方式、參數,如何優選激發、接收環境,如何保證不同激發方式的資料能正常拼接; 4 、山前帶巨厚礫石區的表層結構調查技術及靜校正方法研究。
  6. Hengshanbu part have three secondary parts which are tiekesumiao, eastern taole and south of selunkademiao. the zhouzishan part of is charactered by thrust nappe which is composed by faults thrust from west to east, anticlines and synclines, involving much of proterzoic, palozoic and very limited mesozoic in which a suite of conglomerate is found in the front of thrust fractures in late - jurassic

    桌子山段以發育一系列由西向東逆沖的斷裂和背向斜組成的推覆體系為特點,捲入地層多為元古界-古生界,中生界分佈有限,其中晚侏羅世地層在逆沖斷裂前緣普遍見一套礫巖,故測該段逆沖構造形成於晚侏羅世。
  7. 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 、盆地燕山期構造界面上下不同構造層具有完全不同的構造樣式,構造界面下伏構造層呈現沖斷褶皺、構造樣式,構造界面上構造樣式為階梯狀正斷層,整呈現「雙層」結構型式。
  8. The formation of the nappe led to sinking of qaidam massif, nappe thrusting basin depositing persistently and the sedimentary center changed

    構造的形成,導致柴達木地塊下沉,推覆體持續逆沖盆地持續沉積,沉積中心也變更。
  9. The nappe structures made the faultage in this area developed. the faultage is along or close to meridional direction, and it offered favorable conditions for the formation of the mineralizing fluid

    構造使得該區斷裂、斷層發育,主要以南北向或近南北向斷裂為主,斷裂帶的發育為流的形成提供了有利的條件。
  10. The study on the structural feature opened out by the non - seismic ( mt ) profile of xiaonangou in qinglong mountain on the west edge of ordos basin and the seismic profile across helan mountain shows that a series of thrust blocks - qinglong - luoshan - nioushou - helan mountain, were the thin - skin structure formed by the westward compression of ordos block and the dextral shear of alashan block

    通過對盆地西緣青龍山南端小南溝的非地震mt剖面以及橫穿賀蘭山的地震剖面揭示的構造形態研究認為,盆地西緣一系列推覆體青龍山?羅山?牛首山以至賀蘭山是由於鄂爾多斯地塊向西擠同時與阿拉善地塊的右行運動所產生的「薄皮構造」 。
  11. From hydrogeology the authors study distributive characteristics and hydrogeological characteristics of nappe gneiss, mineral water quality and reserves, theoretical feasibility of developing gneiss mineral water and the problems which remain to be researched

    從水文地質角度,對推覆體片麻巖的分佈特徵、水文地質特徵、水質及儲量進行分析研究,從而提出開發片麻巖礦泉水的理論可行性和有待于進一步研究的問題。
  12. The mineralizing fluid in lanping - baiyangping area is deep circulatory thermal brine as a whole, the mineralizing matter mainly comes from deep, and the genetic type of the deposit belongs to the low - to - moderate - temperature hydrothermal silver polymetallic ore deposit related to nappe structures

    因此,蘭坪白秧坪地區成礦流為深部循環的熱鹵水溶液,成礦物質主要來源於深部,礦床成因類型屬于與構造有關的中低溫熱液銀多金屬礦床。
  13. Elementary analysis on breaking feature of overburden rock during mining under special nappe structure

    特殊推覆體下開采巖破壞特性淺析
  14. Coal is mined under nappe in xinji mine area

    新集礦區是從推覆體下採煤。
  15. Study of seam structure characteristics under large and extra thick nappe

    大型特厚推覆體下煤層構造特徵的研究
  16. Mining practice on fully mechanized coal mining face in island under dumping overburden

    推覆體下孤島綜采工作面開採的實踐
  17. Back - sliding nappe

    后滑推覆體
  18. Destructive study of the cover rock relating to the fully mechanized mining with caving method under ravelly ground and nappe

    鬆散層及推覆體下綜放開采巖破壞研究
  19. The zijinshan fluid system and the gonglang fluid system were driven by the stress of extrusion nappe onto the basin and the thermal driving force of magmatism. when the fluids cycling in the basin encountered the boundary of reduction - oxidation or underwent fluid mixing, phase separating and fluid boiling caused by fault - induced pressure reducing, the physical chemistry condition abruptly changed and mineralization then took place

    在盆地兩側擠壓構造應力及巖漿作用熱力驅動下,紫金山背斜和公郎弧兩大流系統的流在盆地中運動,當遇到氧化還原界面或遭受流混合、相分離及斷裂導致的減壓沸騰時,因物理化學條件發生重大變化而導致成礦作用的發生。
  20. The study objects of the paper are used in different stage of the design process in the design method. it is to say that after the target performance level is selected, the deformation control design method is used as the structural design method ; the static push - over analysis method is used as the structural nonlinear calculation method and the capacity spectrum method is used as the structural performance evaluation method. so the unified structural design method of the performance based aseismic design can be formed and the aseismic performances of the structures can be controlled in every step of the design process

    該方法將本文研究的各方面內容綜合應用於結構設計的不同階段,即在結構選擇了合適的抗震性能等級后,採用結構變形控制抗震設計方法作為結構的設計方法,以結構靜力( pusheseeover )分析方法作為結構的計算分析方法,以結構抗震性能評估的能力譜方法作為檢驗結構實際抗震性能的評估與驗算方法,形成統一的結構抗震設計方法,在結構設計的各個階段控制結構的抗震性能,現基於結構性能的抗震設計理念。
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