盆地區 的英文怎麼說

中文拼音 [péndeqū]
盆地區 英文
cuvette reg. de la
  • 盆 : 1. （盛東西或洗東西用的器具） basin; tub; pot 2. （姓氏） a surname
  • 區 : 區名詞（姓氏） a surname
  1. Basin evolution and hydrocarbon potential in songpan - aba area

    阿壩地區盆地演化及油氣遠景
  2. On the basis of analogic methodology, the deep gas resources of the basin is evaluated as 1116. 144 billion cubic meters, which is mainly distributed in the zones of xujiaweizi, miaotaizi, changling, yingshan, and gulong

    根據松遼盆地深層天然氣區帶地質評價參數取值標準，進行區帶地質評價，並通過與刻度區類比，得出深層天然氣資源量為11161 . 44 10 ^ 8立方公尺，主要分佈在徐家圍子、廟臺子、長嶺、鶯山、古龍等區帶中。
  3. A preliminary report of cultivar introduction and cultivation of potting anthurium in nanjing

    南京地區盆栽紅掌引種栽培初報
  4. The method has triumphantly applied in sag evaluation in chagan depression, and enhanced the forecast of exploration targets, and achieved favorable effect, and auspicated a new way of exploration for similar lower exploration mid - small basins

    該方法成功地應用於查干凹陷的凹陷評價中，提高了勘探目標的預測能力，獲得了良好效果，為類似中小盆地的低勘探程度地區的勘探創出了一條新路。
  5. Under the guidance of theories of sedimentology, petroleum geology and sequence stratigraphy, and through the comprehensive analysis of outcropsrock, cores, well logs and testing outcomes of rock gas, this paper studies the depositional systems of neopaleozoic and the character of aeration zone in tabamiao area of ordos basin. the result indicates that the object layers are divided into two depositional systems, the barrier seacoast depositional systems are recognized on upper carboniferous taiyuan phase with tidal flat, lagoon and barrier bar sedimentary deposit

    本文根據沉積學、石油地質學和層序地層學理論，綜合利用地表露頭、鉆井巖芯、測井曲線資料和試氣成果資料，對鄂爾多斯盆地塔巴廟區塊晚古生代沉積體系及含氣層特徵進行了研究。結果表明，研究區內目的層段可以劃分為2個沉積體系： （ 1 ）上石炭統太原期為有障壁海岸沉積體系，發育潮坪?瀉湖?障壁砂壩沉積。
  6. 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，研究了各構造層的構造特徵：基底構造層：受早海西期構造作用的影響，與準噶爾洋盆俯沖閉合、而後陸-陸碰撞的區域擠壓構造作用有關，為一構造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構造有關的構造-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。
  7. Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock

    摘要以現有資料為基礎，通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究，認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化，沉積了巨厚的新生代地層，自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。
  8. Yitong basin is a big inland basin which was formed in cainozoic. chaluhe depression, which lies in the yitong, is a promising area for long - term oil and gas reservoir exploration

    伊通盆地是一個較大的新生代內陸裂陷型盆地，其中的岔路河斷陷為中長期油氣儲量接替勘探區。
  9. Furthermore, the dq value ranges of profile multifarctal spectra in different landform types and in different directions of the same sections perform different properties and anisotrpies. it can be concluded that the landscape fractal properties depends closely on the int ensity, manner and inhomogenity of exogenic and inogenic processess, and with the properties, we can study quantatively the dynamic geomorphic process. by using the same methods just above, local fractal dimensions d, crossover length tc and the multifractal spectra dq - q of two large - scale landform profiles ( across and along tianshan mountain ranges respectively ) are calculated. the results show that in the studied scaling range the two profiles perform different scaling properties, and both of them can be divided to three evident different linear scaling subsections

    不同類型地貌區二維地貌表面也表現出多度域分形特徵，而且隨著觀測尺度的增加，每個區間的分維值均表現為依次減小，表明外營力作用的影響逐漸被內營力作用所取代：不同類型地貌區在相應區間的分維值表現為高山區中低山區盆地區，體現了不同類型地貌表面粗糙性或復雜性的差異，因此分維值大小可作為地貌表面外營力侵蝕作用強度的重要指標：利用標度區的間斷點和各種地貌類型表面分維值或宏觀效應趨於一致，提出5 - 6km左右可作為地貌的宏觀臨界點，並且與利用地貌剖線研究所得到的5km這一數值是基本吻合的。
  10. In addition, the dq - q curves behave in different shapes. it can be concluded that the scaling properties depend colsely on the way, intensity. acting scale and distribution in space of inogenic and exogenic processes. according to the scaling natures of the two landform profiles, it is proposed that the 5km scale is the low limit of the inogenic process effects which begin to dominate landscape patterns in landform systems

    該結果對理論地貌研究具有重要意義：不同地貌類型表面的多重分形譜值域表現為高山區中低山區盆地區的總體特徵，地貌表面多重分形譜特徵表明了內外營力地貌作用類型和強度在空間上分佈的不均勻程度。
  11. Case study of a regional heavy rain over northwestern qinghai province

    柴達木盆地區域性中到大雨個例分析
  12. The "dust bowl" covered one hundred countries.

    這一「灰盆」地區延伸達100個縣。
  13. 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。
  14. After that, the multifractal spectra dq - q are computed by fixed - mass method. the results show that in the studied scaling range different types of landscapes and profiles in different directions perform different fractal properties, that is, the d value and crossover length ^ decrease in turns with the landform type from high - moutain, mid - low mountain to basin, and the profile parallel to wear grooves often has lower d values ( < 1. 5 ) than those perpendicular to wear grooves do ( 1. 5 ) in the same section

    提出以地貌分形特點和渡越長度為依據的地貌層次界定方案，研究指出了5km左右應為宏觀臨界點：不同構造地貌區、不同取向的剖線的多重分形譜值域范圍寬窄表現出中低山區高山區盆地區，垂直構造地貌斜坡方向斜交方向平行方向的特點，表明了內外營力作用的不均勻性和方向性。
  15. Breakthrough in mineral exploration using geogas survey in the basin area of northern qilian region and its significance

    地氣測量在北祁連盆地區找礦突破及其意義
  16. By using the standard deviation method, the scaling properties described by the local fractal dimension d and crossover length tc of 48 measured landform profiles in different direction of 6 different studied landform sections are calculated

    負反饋機製表現的越明顯；對于以構造沉降作用為主的盆地區而言，各個方向的地形剖線的分維值均顯示出小於1 . 5的正反饋機制。
  17. In this area, there are obviously different crustal tectonics within the basins and mountains displaying that the thickness of crust in the mountain areas is greater with obvious " mountain root " and thinner in basin areas

    已有資料表明，在中國西北盆山地區，山脈和盆地具有明顯不同的地殼結構，它們的地殼厚度不同，表現為山區地殼厚，具有明顯的山根；盆地區地殼厚度小。
  18. In conclusion, it tables a proposal that it divided the sichuan into three sections : the basin section, the mountainous area in the southwest sichuan, the altiplanos section in the western sichuan then it recommends the pavement structure applied to different nature climate condition and different grade highway

    本文針對四川省高等級公路路面結構的使用情況，並對以後的發展作了展望，提出了把四川省劃分為盆地區、川西南山區、川西高原區三個分區，推薦了適用於不同自然氣候條件和不同等級公路的路面結構。
  19. ( 2 ) in southern china, the velocities are near average value. a little low velocities exist in the regions such as zhujiangkou, middle of guangxi, lushan and so on. a little high velocities exist in the middle region lied to the south of yangzi river and to the north of zhujiang river

    東部地區速度變化以低速異常為主：整個華北和東北地區，都呈現pn低速異常，特別是華北盆地區、渤海灣和山西地塹低速異常非常明顯，最小低於7 . 8km / s ；華南地區整體上在平均值上下，在珠江口地區、廣西中部地區、廬山地區波速略微偏低，在長江以南，珠江以北地區中部波速略微偏高。
  20. Depending on the data of the new oil and gas resources survey, the subsidence history and structural evolution of north yellow sea basin are emphatically analyzed in this paper based on the brief discussion on the characteristics of tectonic geology of north yellow sea basin

    摘要依據最新油氣資源調查資料，在簡述北黃海盆地區域構造特徵的基礎上，重點分析了盆地的沉降史與構造演化特徵。
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