沉積形成 的英文怎麼說

中文拼音 [chénxíngchéng]
沉積形成 英文
sludge formation
  • : 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動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. The pathology characteristic that liver fiber changes is collect there are many fibre hyperplasia and deposit inside abbacy and liver flocculus, but have not form the interval inside flocculus, liver cirrhosis has false flocculus to form, central vein area and collect abbacy occurrence interval, the normal structure of liver is destroyed, liver fiber changes further progress to be liver cirrhosis namely

    肝纖維化的病理特點為匯管區和肝小葉內有大量纖維組織增生和,但尚未小葉內間隔,肝硬化則有假小葉,中心靜脈區和匯管區出現間隔,肝的正常結構遭到破壞,肝纖維化進一步發展即為肝硬化。
  2. The sedimentation is the foundation, affecting the basic pattern of the reservoir, and the sedimentary facies zones beneficial to the formation and evolution of the reservoir includes platform edge bank facies, introplatform point beach facies and acclivity sedimentary facies, etc. ; the diagenesis is the key factor, determining the pattern and scope of the final distribution of the reservoir and being of great influence on reservoir structure, and the diagenesis of promoting the formation of storage rooms is mainly the dissolution occurred during hypergene stage and burial stage ; and the tectonism is the condition of influencing the connectivity among various reservoir bodies and among the storage rooms within a single reservoir body

    該套儲層是在4億年左右的地質歷史中,由巖和構造作用相互影響而的最終果:其中作用是基礎,影響著儲層的基本態,有利於儲層與演化的相為臺地邊緣灘、臺內點灘和上斜坡等相帶;巖作用是關鍵,決定了儲層的最終分佈態和范圍,對儲層結構的影響至關重要,促進儲集空間巖作用主要有表生期和埋藏期的溶解作用;構造作用是條件,影響著各儲集體之間以及單一儲集體內部儲集空間的連通情況。
  3. Sedimentary control of coalbed methane in this region were expounded according to the control and influence of sedimentation on coal gathering action ( thickness of coal reservoirs, distributing and coal - bearing characteristics ), on forming and distributing, maceral, organic facies and coalfacies, cap formation types and their sealing capability of adjoining rock

    根據作用對聚煤作用(煤儲層的厚度、分佈及含煤性特徵) ,對煤儲層的與展布、煤巖組、有機相和煤相、頂底板蓋層類型與封蓋性能的控制和影響,討論了作用的控氣特徵。
  4. While working, the air with dust enters into the sedimentation chamber via wind entrance, dust with large size granule will fall because of sudden expand of the aeriform cubage, then the air will pass the water area of arc boards of the two sides to stir the water. then air with dust will be mixed with water forming water curtain at the exit, fine powder will be collected, purified air will be discharged by blower fans via breakwater and wind exit

    工作時含塵空氣從進風口進入降室由於氣體的體驟然膨脹,大顆粒粉塵集下來,然後空氣經過兩側弧板間的水域並將水攪動含塵空氣與水充分混合在出口處水幕,較細的粉塵捕集下來,凈化后的空氣經擋水板和出風口由風機排走。
  5. ( 1 ) the soil from century garden is an alluvial and diluvia soil in an alkalescent medium

    ( 1 )世紀花園地基土是在弱偏堿性介質環境下的沖洪
  6. Three main rock types make up the geology of singapore : igneous, sedimentary and alluvium. where is the main source of granite found

    新加坡地質的三種主要巖石類型:火巖、巖和沖巖。哪裡是花崗巖的主要來源地?
  7. These tiny debris-flow deposits formed on freshly excavated embankments of the california aqueduct.

    這些細小的泥石流是在新開鑿的加利福尼亞渠的大堤上的。
  8. In the research area, the incised valley was formed during the sea level downwards and was provided source by the arenaceous river from qiaotou. it is stacked by 3 incised valleys formed in 3 different sequences

    研究區內子洲鎮川堡地區發育的下切河谷於海平面下降時期,來源於橋頭的砂質河流,為疊置的、於三個不同三級層序底部的下切河谷充填
  9. By infrared spectrum study, the limonite ( feooh nh2o ) can be considered the main colorating mineral in the yellow and red jadeite, and the hematite is another colorating mineral in the red jadeite. the difference of color tone is due to the n value in the molecular formula feooh nh2o and the content of crystal water and adsorbent water. the iron ion came from the effloresced and eroded rocks, and formed fe ( oh ) 3 colloid reacted with the surface water

    周圍礦床的風化蝕變為表生水提供了鐵質,弱酸性的含fe ( oh ) _ 3膠體的水溶液,表生水流經翡翠礦石時, fe ( oh ) _ 3膠體附著在巖石的表面,經過脫水結晶和吸附,褐鐵礦膠體,褐鐵礦膠體沿裂隙或鬆散的礦物顆粒進入翡翠巖石中,逐漸累澱,次生色層。
  10. On this surface the encroaching muskeg sea developed a carbonate bank fringed by coastal sabkhas in which gypsiferous deposits were formed.

    在這個地表上,侵入的馬斯愷格海發育了一個碳酸鹽灘,其邊緣有海岸薩勃哈石膏質沉積形成
  11. In middle and late periods of the early permian, the pre - caspian areas rose successively, the climate became dry, and the environment turned to be supratidal zone ( evaporitic environment ), resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite

    早二疊世中後期由於持續構造抬升,盆地氣候變得乾旱,海水變淺,潮上帶蒸發環境發育,以致這一時期廣泛發育鹽類含鹽層系,主要由鹽巖和硬石膏層構,並許多大小不等的鹽丘構造。
  12. The alternative changes of paleoenvironment favored the formation and imbedding of brine, which is the source of salt - water intrusion ; and the paleochannel that formed during regressive of sea level is the path of salt - water intrusion

    海進時期,大面的濱海平原被淹沒,在近海平原窪地滯留的海水經過蒸發、濃縮變為鹵水,為鹹水入侵的物源;海退後陸源碎屑在濱海地區沉積形成了巨厚的古河道砂層。
  13. The oldest exposed rocks are devonian fluvial sediments that were deposited 400 million years ago. the region was subsequently inundated by a shallow sea

    年代最久遠的巖石是四億年前泥盆紀時期由河流沖巖。
  14. Hong kong lies on the southern edge of an ancient land mass. the oldest exposed rocks are devonian fluvial sediments that were deposited 400million years ago

    香港處于古陸塊的南緣,最老的外露巖石是在4億年前的泥盆紀時期,由河流沖巖。
  15. Standard test method for vehicle evaluation of unleaded automotive spark - ignition engine fuel for intake valve deposit formation

    進液閥門沉積形成的不含鉛自動火花點火引擎燃料的車輛評價標準試驗方法
  16. Based on the principles of palaeobiology, stratigraphic geology, sedimentology, diagenesis and reservoir geology, taken field profile and drilling cores as research object, and combined with achievement of predecessors, the sedimentary facies, diagenesis essential characteristics of reservoir and controlling factors for reservoir of feixianguang formation in northwest sichuan have been comprehensively studied. both classic and mordern methods have been used in this research. the main confents includes : stratigraphic classification and correlation of feixianguan formation in lower triassic, the rock fexture characteristics, type and forming conditions of rock ; determining dirtributary law of the sedimentary facies in vertical and horizontal direction and distribution in plane and the essetial contronling factors through correlation of sedimentary facies transverse profile and regionnal geologic characteristics ; establishing plane stereoscopic modle of sedimentary of oolitics beach by studying diagenesis

    主要內容包括:對川西北地區下三疊統飛仙關組地層進行了劃分與對比,研究了飛仙關組地層的巖石結構組分特徵、類型和條件;通過相橫向剖面的對比,並結合區域地質特徵,深入研究了相在縱、橫向上的變化規律,確定了相在平面上的分佈及主要控制因素,分析了相的縱向演化過程和建立了相的平面立體模式;詳細研究了該套地層所經歷的巖作用類型、特徵及對儲集空間的影響,建立了鮞粒灘相儲層的與演化模式;最後,從相、巖作用的角度,分析了區內飛仙關組地層的生油潛力、儲層的分佈規律和發育區塊。
  17. The analysis shows that, compared with mineral and chemical component content, the granularity fractal characteristics have higher correlative degrees with slaking durability, which reflects that the deposit environment influences slake durability deeply than other factors

    分析發現,與分相比,紅層軟巖的粒度分佈分特徵參數與崩解特性具有更高的關聯度,表明沉積形成時的環境決定了巖后的紅層軟巖崩解性強弱。
  18. The nasa team had hoped spirit would find equally clear signs on the ground : things like the sort of rounded pebbles or boulders found in terrestrial river beds, ripples in the sand, or rocks built up over time by the deposit of sediments from water

    Nasa的工作人員希望「勇氣號」能在地面上找到對等的痕跡,如:河床上的圓鵝卵石或漂石,沙灘上的波紋,經過長時間由水中澱物的石頭。
  19. Significant research works have been focused on single metal, in particular copper deposition and its mechanism and kinetics, including electrochemical parameter and physical parameter measurements

    研究了單金屬特別是銅的機理和動力學以及採用的研究方法和分析測試手段,包括對電化學參數和物理參數等研究。
  20. The long - term base - level cycle comprises the third and the fourth section of shahejie formation, which are successive, and the fourth section is rising term of the long - term base - level cycle ; the underside of the fourth section of shahejie formation is the fangshenpao formation, and their interface is a unconformity

    研究區沙四地層與上覆的沙三段為連續一個完整的長期旋迴,而沙四為長期旋迴的上升期;沙四與下覆房身泡組為不整合接觸。
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