隆起區 的英文怎麼說

中文拼音 [lōngqǐqū]
隆起區 英文
upwelling area
  • 隆 : 隆Ⅰ形容詞1 （盛大） grand2 （興盛） prosperous; flourishing; thriving 3 （深厚; 程度深） deep; in...
  • 起 : 起Ⅰ動詞1 （站起; 坐起） rise; get up; stand up 2 （取出; 取走） draw out; remove; extract; pull 3...
  • 區 : 區名詞（姓氏） a surname
  • 隆起 : [地質學] rise; tuberositas; bulge; protuberate; eminentia; hump; uplift; upheaval; heave; intumes...
  1. Based on analysis of geologic foundation record about pingzhuang basin, a lot of sino - foreign geothermal geology record and investigation of field geology, measuring of ground temperature in person and geo - chemical analysis of ascension spring, gushing water of fault, the fact that the anomaly of geothermal gradient of pingzhuang basin, which is in region of low geothermal gradient, is caused by redistribution of conduction - oriented geothermal heat flow which is result from upheaval and depression of basin foundation bed is pointed out. after the field of ground temperature is simulated under the background of conduction - oriented geothermal heat flow by means of ansys, the characteristic of ground temperature distribution of top surface of basin foundation bed ( yixian team ) is revealed. the sound condition of transmissibility fault and feeding water source, which are imperative in formation of the low - medium temperature geothermal system of convective type, is possessed in pingzhuang basin

    通過對平莊盆地基礎地質資料、國內外大量地熱地質資料的分析和野外地質調查、礦井實測地溫以及上升泉、斷層涌水的地球化學分析等工作基礎上，指出地處低地溫梯度背景區的平莊盆地地溫梯度異常是由於盆地基底隆起和坳陷引起傳導型大地熱流再分配所致；運用州sys數值模擬了大地熱流向地表傳導背景下的盆地地溫場，從而揭示了盆地基底（義縣組）頂界面地溫分佈特徵；闡明了盆地具有形成中低溫對流型地熱系統所必需的導水斷裂、補給水源等的良好條件，中低溫對流型地熱系統是地熱勘查的主要對象；圈定了平莊盆地北部朝陽溝?駱駝營子地熱勘查遠景區。
  2. Based on the geological, hydrogeological and hydrochemical information, the genesis of the underground hot water in qi county of shanxi has been analyzed. it is concluded that the formation of underground hot water is related to the magmatic activity in yanshan period, the goup of the base fault block forming in new tectonic period, the large depth and fast variety to underground water cycle

    從地質、水文地質、水化學等方面，分析了祁縣地區地下熱水成因，得出該地區地下熱水形成與燕山期巖漿活動、新構造運動形成的基底斷塊隆起及地下水循環深度大、交替迅速有關。
  3. Intermontane basins in relatively stable regions subjected to regional uplift.

    較穩定區域內的山間盆地，曾有過區域隆起。
  4. Mount sainte - genevieve formed an enormous mound to the south ; and it was a sight to see from the summit of notre - dame how that throng of narrow and tortuous streets ( to - day the latin quarter ), those bunches of houses which, spread out in every direction from the top of this eminence, precipitated themselves in disorder, and almost perpendicularly down its flanks, nearly to the water ' s edge, having the air, some of falling, others of clambering up again, and all of holding to one another

    聖日芮維埃芙山像一個巨大圓瓶兀自隆起在東南邊，這倒是很值得從聖母院頂上觀看一下的:只見那許許多多狹窄彎曲的街道（今天的拉丁區） ，那密密麻麻的屋宇，從山頂上向四面八方撒散開來，幾乎一溜筆直地沿著山坡俯沖下去，直至河邊，有的像要跌倒，有的像要再爬起來，但又都似乎彼此相互扶持。
  5. In prophase there existed thermal and magma activity, and before the

    其下為一火成巖體隆起帶，之下有更深部的熱力作用區。
  6. In east china sea shelf basin, the mesozoic relict sediments are distributed in some central - south areas, such as fuzhou sag, minjiang sag and yushan lower uplift

    摘要東海陸架盆地中生界主要分佈於盆地中南部的福州凹陷、閩江凹陷和漁山低隆起地區。
  7. Results the result on this sedimentary environment was an offshore terrigenous fresh water lake from permian of shiqanfeng formation marinecontinental transitional facies in the southern of north china

    結果研究區地層自南西向北東呈現依次增厚的趨勢，整體為北東方向傾斜的寬緩斜坡環境；砂巖分佈特徵指示物源來自南部隆起區和沉積中心在研究區以北地區。
  8. The paper discusses dynamical conditions of the supercritical ore - forming fluid system based on study of regional geological background and analyses of physiochemical conditions of ore - forming process and puts forth the ore - forming mechanism : upper mantle uplift - mingling of meteoric water and magmatic hydrothermal fluid separated from acidic magma under tensile or transitional tensile environment - water / rock reaction - transportation - chemical coupling ore precipitation

    在分析超臨界成礦流體系統形成的區域地質背景和研究成礦物理化學條件的基礎上，探討了超臨界成礦流體系統形成的動力學條件，提出該系統的成礦機理：與燕山晚期酸性火山侵入巖漿有關的金銅礦床是在上地慢隆起、張性或向張性過渡背景下形成的，酸性巖漿經熔體流體分離作用形成的巖漿熱液與大氣降水混合，經水巖作用等復雜的輸運和化學反應耦合過程的動力學產物。
  9. It is shown that deep abnormal high pressure confined area ( abnormal prressure fluid compartment ) at footwall in southern margin of the basin and uplift sector closely related to faulting should be as a domain or direction for exploration ， and structural traps ( like faulting barrier ， anticline ， etc. ) along with original oil / gas reservoirs at major faulting footwall as the main exploratary targets

    盆地南緣斷裂下盤深層的異常高壓封閉區（流體封存箱） 、與斷裂密切相關的隆起段是今後主要勘探方向與領域，斷裂遮擋、背斜等構造型圈閉? ?主斷裂下盤原生油氣藏是主要的勘探對象。
  10. In the present survey and valuation the area is divided into three parts : exposed karst region in upwarped distric, karst region controlled by folded structures near depressed belts and blinded karst region in fault basins

    目前開展的可有效利用的地下水資源調查評價將該區劃分為隆起帶裸露巖溶分佈區、沉降帶邊緣褶皺構造控制巖溶分佈區和斷陷盆地隱伏巖溶分佈區。
  11. According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin

    依據理論分析及勘探實踐，優選出4個有利的勘探區帶，它們是：庫車前陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉；準南前陸沖斷帶第二、第三排構造帶；川西北部及南部燕山運動期古隆起、川中平緩褶皺構造帶以及深坳陷內部的非常規天然氣；柴北緣冷湖南八仙構造帶。
  12. The authors hold that the joint actions of numerous factors such as the upper mantle uplifted zone ( the mantle thinned zone of lithosphere ), the upper mantle anomalous area ( relatively low - velocity area ), the uplifted zone of intracrustal high - conductivity layer, the deep fault ( shear zone of lithosphere ), the margin of the crust - upper mantle uneven masses, the basement uplifted area reflected by gravity high, the magmatic belt and tectonic intersection reflected by skipped magnetic field, control the distribution of auriferous skarn deposits and copper ( associated with gold ) skarn deposits

    作者認為，上地幔隆起帶（巖石圈地幔減薄帶） 、上地幔異常區（相對低速區） 、殼內高導層隆起帶、深斷裂（巖石圈剪切帶） 、地殼上地幔不均勻性塊體的邊緣、重力高反映的基底隆起區、跳躍磁場反映的巖漿巖帶和構造交匯處等諸多因素的共同作用控制著含金夕卡巖礦床和銅伴生金夕卡巖礦床的分佈。
  13. So it can be concluded that there did not exsit regional compressional folded - uplifted area which was eroded widely in mesozoic in the west neighouring district

    這表明中生代在盆地西鄰不存在廣泛遭受剝蝕的區域擠壓褶皺隆起區。
  14. However, the large - scale erosions in the uplift areas of the fault belt and the surrounding margins allow the determination of the fault active periods to be difficult

    在斷裂帶和外緣的隆起區地層剝蝕程度較大，活動時間的釐定比較困難。
  15. The migration of hydrocarbon tends to take place from high pressure stress distribution area ( hydrocarbon generation sag ) towards low pressure stress distribution area ( uplift )

    油氣從高壓應力分佈區（生烴凹陷）向低壓應力分佈區（隆起區）運移。
  16. The special aerial magnetism, gravity and mt at chasang segment in the western uplifting district show that it is superposed by two or three large - scale south dipping structural block with east - west strike. the closure of bangong lake - dingqing limited ocean and the further gathering of neighboring blocks later form it

    西部隆起區查桑段特殊的航磁、重力和mt顯示其由2 - 3個近東西向大型南傾構造塊體疊覆而成，受班公湖-丁青有限洋關閉和相鄰地塊進一步匯聚形成。
  17. ( 1 ) abnormal high velocities mainly exist around qingzang plateau, especially in junggar, tarim, qaidam and sichuan basin, velocities there are higher than 8. 2 km / s. ( 2 ) low velocities only exist in the middle of qingzang plateau and western part of sichuan and yunnan region. in eastern china, low velocities are predominant

    整體上中國東西部存在明顯差異，西部地區速度變化以高速異常為主：高速異常區主要是沿青藏高原隆起區的周邊分佈，特別是準噶爾盆地、塔里木盆地、柴達木盆地及四川盆地都呈明顯的高速，均超過8 . 2km / s ；青藏高原隆起區的中部，顯示出速度的低異常帶；位於青藏高原東南緣的川滇西部地區速度呈現低異常。
  18. 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標度范圍內，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）沉積凹陷區（盆地區） ；在5 - 200km標度范圍內則表現出強烈隆起區最新隆起區沉積凹陷區。
  19. The regional deformation anomaly of medium - term phase ( 1 ~ 3 years or more ) before strong earthquake occurrence usually shows three aspects of common characteristics : for regional vertical deformation, it shows distribution features of anomalous uplift area and concentration belt - high gradient belt of vertical differential deformation ( some of them reflect distribution of four quadrants ) related to tectonics ; for horizontal movement, it shows features of centralized high strain area ( or zone ) of domination shear deformation related to active blocks and faults ; it shows common features of regional vertical deformation anomaly area and high strain distribution area of horizontal deformation

    摘要強震前中期階段（ 1 ~ 3年或稍長）區域性形變異常往往表現出3個方面的共性特徵：區域垂直運動變形呈現與構造有關的異常隆起區、垂直差異變形高梯度帶（有的還呈「四象限」 ）分佈特徵；水準運動變形呈現與活動地塊及斷裂構造有關的、以剪切變形?主的高應變集中區（帶）特徵；區域性垂直形變異常區與水準形變的高應變分佈區共性的特徵。
  20. It can be inferred that the fractional dimension values are closely dependent on the erosional intensities, and it can be a very important parameter for dynamic geomorphological researches

    隆起區分維值所表現出一般特點是大於1 . 5的類似於準周期運動的負反饋機制。侵蝕作用的強度越大。
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