沉陷度 的英文怎麼說

中文拼音 [chénxiàn]
沉陷度 英文
settlement
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : Ⅰ名詞1 (陷阱) pitfall; trap2 (缺點) defect; deficiency Ⅱ動詞1 (掉進) get stuck or bogged do...
  • : 度動詞[書面語] (推測; 估計) surmise; estimate
  • 沉陷 : 1. (下陷) sink; cave in 2. (沉降) sinkage; downpunching; depression; subsidence; [建築] settlement
  1. Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area

    詳細的積相研究發現,紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要積相類型,並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的積相平面編圖,以較高的時間解析揭示了區內積相帶的平面展布及其在不同構造背景中的分佈規律,比如在北部的凹陡坡背景下,上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的積體系,下降半旋迴高水位期,扇三角洲相粗碎屑巖由北向南進積;在南部的凹緩坡背景下,上升半旋迴主要發育辮狀河流相,下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相積和鹽類積。
  2. By physiognomy feature, it could be divided into three types of thermal structure : positive dome model, negative collapse model and border dome core collapse model. based on the depth degree or magma - thermal influenced, it could be divided into five types of thermal structure : ( ancient ) geothermal anomaly focus region model, superficial volcano eruption hydro - thermalism and hypabyssal intrusive model, thermal anticline ( thermal dome ) model, mid - deep intrusive model, deep mantle ( crust ) thermal plume model ; and put forward a perfect model of the thermal structure. there are many interaction system could be induced into a systematic thermal interaction, include : ocean - continent system, basin - mountain interaction, superficial and mid - deep crust - mantle interaction, crust - mantle commingle interaction, vertical thermal interaction ( delamination ) etc.

    依據地貌形態分為三類:正向穹窿型、負向塌型、邊隆核型:依據巖漿-熱力作用影響的深淺程或深分為五類: (古)地熱異常群集區、表淺層火山噴發-熱液活動與淺成侵入型、熱力背斜(熱穹窿) 、中深層侵入型、深部地幔(地殼)熱柱型;提出了熱力構造作用空間分佈的理想模式,將洋陸系統、盆山作用、淺表與中深部殼幔作用、殼幔混合、垂向熱力作用(拆)等納入一個整體統一的熱力作用系統中,為盆地動力學研究打開了一個新窗口;研討了熱力構造研究方法。
  3. The dependence of oxygen precipitation and induced - defects in heavily as - doped silicon on heat treatment process was studied by annealing and ig process, chemical etching, scanning electron micrograph ( sem ) and transmission electron microscopy ( tem ). a developed ig technique was suggested and the mechanism of the influence of as on oxygen precipitation formation in heavily as - doped silicon was discussed

    本文通過化學腐蝕、光學顯微鏡、掃描電鏡( sem ) 、透射電境( tem )等分析技術,對重摻砷硅單晶在單步退火工藝和內吸雜退火工藝中氧澱及誘生缺的形態,形核與熱處理溫、時間的關系等進行了研究。
  4. 4 ) the characteristic of tricyclic terpane reflected the source input of algae. the predominance of 4 - methylsterane and dinosterane, and the c _ ( 27 ) - sterane predominance " v " distribution pattern all indicate the great contribution of algae source input. based on the ratio of sterane c2920s / ( 20s + 20r ) and c29 / ( + ), the source rocks can be regarded as typical immature source rocks

    2 、利用豐富的生物標志化合物信息,分析解釋了生源構成、積環境、有機質演化等特徵,表明德南窪主力烴源巖的生源構成是以菌藻類微生物為主且含有一定陸生植物輸入的混合生源,積環境為半鹹水-鹹水還原環境,積水體具有「層狀」特點,表層鹽高,底層還原性強。
  5. The high or low velocity anomalies ' s locations are consistent with the uplift and depression respectively, and their contacting boundary always correspond the faults exposed on the ground ' s surface. the basement interface that is the bottom interface of the sedimentary cover undulates strongly

    上部地殼高速異常和低速異常分別與地表的隆起和坳一致,高速異常和低速異常的接觸帶往往與地表的斷裂位置有良好的對應關系,積蓋層底部的基底界面橫向上起伏變化較大。
  6. Gully erosion, which is universal on original lands, but also the special forms, for example, hole erosion gravel erosion debris slide and debris flow, which is unusual in loess area, ( 2 ) based on a long - term fixed point experiments in proving ground of the south stackpile, the soil erosion factors have been researched quantitatively, the runoff and erosion affected factors have been made sure and the experiential models of producing water and soil have been taken in newly - constructed stage, early stage and later stage of reclamation

    確定南排土場原地貌的水蝕模數為3700 4400t km ~ 2 ? a ;在排土場新造地貌上,擊濺、面蝕、細溝侵蝕、淺溝侵蝕、侵蝕、砂礫化面蝕、土砂瀉溜和坡面泥石流等水土流失形式出現頻率和發生程都明顯強于原地貌。 ( 2 )以南排土場徑流試驗場長期的定位觀測為基礎,對排土場未復墾時期、復墾初期、復墾後期的土壤水蝕影響因子進行定量研究,確定了徑流和土壤水蝕的主要影響因子及其臨界值,建立了產流產沙的經驗模型。
  7. Being primarily controlled by northwest faults, cretaceous of jiyang depression contained several isolated basins, and lake levels of these isolated basins were instable, but on the whole, shore and shallow lake sub - facies is in the majority

    北西向斷層的活動對積起到主要的控製作用,在其控制下,白堊紀濟陽坳為一相互分割的山間盆地,湖盆范圍時大時小,湖水深不斷變化,總體湖水較淺,主要發育濱淺湖亞相。
  8. It is found that the degree of mineralization and metamorphic coefficient and conversion potential of formation water, the fault is zone of sluicing of atmospheric infiltration water flowing from basin west margin to east ( centripetal flow ) and sedimentary compaction water flowing from qija gulong depression to west ( centrifugal flow )

    通過地層水礦化和變質系數等參數的分佈規律及一系列折算水位剖面圖的分析發現,該斷裂對水是不封閉的,並且是盆地西緣大氣滲入水向東流動(向心流)及齊家古龍坳積壓實水向西流動(離心流)的共同泄水帶。
  9. The experimental results showed that high density of oxygen precipitation and induced - defects were formed after annealing of wafers at moderate and high temperatures

    重摻砷硅單晶在中高溫退火時形成密較高的氧澱及誘生缺
  10. The fractal dimensions of elevation isolines in 6 studying sections from 3 different types of geomorphological zones, including high mountain, low - moderate mountain and catchment basin, are computed by using successive coarsening method. the results show that all the studied isolines are statistical fractals, and the fractal dimensions take on different characters for different geomorphological types and scale ranges

    在0 . 1 - 10km標范圍內,等高線分維值總體表現為最新隆起區(中低山區) >強烈隆起區(高山區)積凹區(盆地區) ;在5 - 200km標范圍內則表現出強烈隆起區最新隆起區積凹區。
  11. Many domestic and overseas cases of surface subsidence and damage induced by underground water mining are enumerated in this paper and the surface subsidence mechanism induced by underground water mining is analyzed from the location of water - bearing stratum, physical characteristics of carrier, drifting manners and subsidence styles

    摘要列舉了國內地下水開采造成地表和損害的許多實例,並從地下水所處的地層層位、載體物性、載體厚、抽排方式和類型入手,分析了地下水開采地表發生機理。
  12. Whereafter, based on the analysis on the flood influence for traffic lines, the research is centered on the following parts : firstly, the destroying modes, reasons and mechanism of flooded lines are discussed, and the frameworks and countermeasures of preventing and controlling hazards system are put forward ; secondly, the ways of region forecasting for the landslide are analyzed and the automation of landslide forecast for certain site through visual programming is realized. furthermore, the function of dynamic segmentation in arc view is made use of to realize the forecast result ' s visualization ; thirdly, the reasons and patterns of roadbed subsidence are discussed and the methods of forecasting subsidence based on the gm ( 1, 1 ) model are put forward. then the applications of the arcview software and its extended module on the study of roadbed subsidence are debates upon ; fourthly, an analysis on the sources of flood for traffic lines, which situate in the reservoir coverage area, is given

    接著,論文探討了山區交通線路災害的特點、分類、時間和空間分佈規律以及災害的防治原則和對策等;然後,以洪水災害對交通線路的毀壞為主線,重點研究和分析了以下幾個問題:第一,探討了洪水對交通線路的破壞方式,水毀原因以及水毀機理,並提出了交通線路水毀防禦系統框架和對策;第二,分析了雨季邊坡塌方災害的區段預測方法;通過可視化編程,編制了雨季邊坡塌方災害的工點預報程序,並結合arcview實現了預測結果的可視化;第三,對路基原因和模式進行了分析,並提出利用gm ( 1 , 1 )模型對路基區進行分析和預測,最後論述了arcview軟體及其擴展模塊在區研究分析中的應用;第四,對汛期庫區線路災害的原因進行了分析,並探討了利用數量化理論對路基防護工程抗洪能力進行預測的意義;第五,提出從風險的角對交通線路的防災減災進行管理,對風險估計的相關問題進行了論述,並探討了交通線路水害危險區段的劃分問題。
  13. While taxpayers who suffer losses in their businesses may be helped to a certain extent to tide over difficult times by loss carry - back arrangements, this would place enormous pressure on tax revenue during periods of economic downturn

    至於本年虧損轉回的寬免,雖然在某程上可幫助業務有虧損的納稅人過經營困難的時期,但在經濟入低潮時,會對稅收造成重壓力。
  14. Associated with the study of lighter hydrocarbon constituent, carbon isotope, biomarker and inclusions, adopted the technique of oil source correlation on whole oil samples, it can be confirmed that the hydrocarbon source of viscous crude in permian, in the east slope of jimusaer depression, is pingdiquan formation mudstone ; carboniferous oil comes from carboniferous source rock. meanwhile, the causes of oil formation are investigated based on datum of reservior geochemistry : viscous crude of permian is the result of biodegradation and low maturity working together, and that lighter hydrocarbon constituent of carboniferous oil is missing. at last, the mode and mechanism of the oil pool formation are analysed in the study area according to the structure phylogeny, sedimentary history, and data of reservior geochemistry

    本論文根據輕烴、碳同位素、生物標志化合物等資料,運用全烴地球化學油源對比方法進行油源對比,得出吉木薩爾凹東斜坡區二疊系的稠油來自平地泉組泥巖,石炭系的稀油來自石炭系本身源巖;同時,根據地化資料研究了原油的成因,認為二疊系稠油是生物降解和成熟較低共同作用的結果,石炭系的稀油存在輕組分散失現象;最後,綜合構造、積、烴源巖和油藏地球化學資料,分析了吉木薩爾凹原油的成藏機制和模式。
  15. The comparatively higher accuracy of the gray forecast method has been proved by the analysis of engineering examples, it is a more practical forecast method of ground subsidence and have a extensive and practical space in engineering

    通過對其工程實例的應用分析,證明灰色預測方法具有相對較高的粉,是一種比較實用的地表預測方法,具有廣泛的工程實用空間。
  16. It is considered that the sedimentary structures of pukou formation in huaiyin nag are different from those in yanfu depression, and the new characteristics of salt rocks of over 1000 m thickness appear in this area

    認為淮陰凹浦口組和鹽阜坳有不同的積構造特徵,特別是本區發育的厚達千米的鹽巖積,更有其特殊性。
  17. Relation between surface subsidence range ' and oeverburd separated

    地表與覆巖離層的關系確定
  18. An example indicates that the updated map, taking on the same data structure with original terrain map and the precision being satisfied with demands of terrain map, can be applied to land planning and mgis used as basic datum

    實例應用表明,更新后的圖形數據結構與原地形圖完全相同,其精滿足大比例尺地形圖的要求,可作為開采區土地規劃和建立礦區地理信息系統的基礎圖件。
  19. A description is made of the problems encountered in gps leveling measurement in this field and countermeasures. as observation of ground subsidence is made through measuring the relative movement of the observation stations, it is proposed to base the subsidence observation on change of geodetic elevation. check is made of the accuracy and reliability of this observation method by citing typical examples

    介紹了gps水準測量中的若干問題及其解決方法,結合開采監測需要的是相對變化量的特點,為避免坐標轉換造成的精損失,提出了開采觀測中的下值可應用大地高的變化量代替的方法,並對其精及可靠性進行了實例驗證。
  20. According to the annual production program, predictted the subsidence by probability - integral method, and then advanced the method that restore the irrigation and draining function of the water system on the ground in the subsidence area, it is changing route of ditch and river system reconstruction

    根據張集礦年開采計劃,對礦區未來可能產生的開采採用概率積分法進行預計,根據預計結果提出了塌區內水系灌溉排澇功能的動態恢復治理方案,即水渠改道和水系重建。
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