第三紀下層的 的英文怎麼說

中文拼音 [sānxiàcéngde]
第三紀下層的 英文
eocene
  • : Ⅰ助詞(用在整數的數詞前 表示次序) auxiliary word for ordinal numbers Ⅱ名詞1 [書面語] (科第) gr...
  • : Ⅰ數詞1. (二加一后所得) three 2. (表示多數或多次) more than two; several; many Ⅱ名詞(姓氏) a surname
  • : 紀名詞(姓氏) a surname
  • : 下動詞1. (用在動詞后,表示由高處到低處) 2. (用在動詞后, 表示有空間, 能容納) 3. (用在動詞后, 表示動作的完成或結果)
  • : i 量詞1 (用於重疊、積累的東西 如樓層、階層、地層) storey; tier; stratum 2 (用於可以分項分步的...
  • : 4次方是 The fourth power of 2 is direction
  • 第三 : third第三帝國 [德國] the third reich (1934 1945); 第三 (層)樓 [美國] third story; [英國] seco...
  1. According to the synthetically study of remnant stratum list, sediment system. character of sediment filling, comeback of archetypal basin and feature of tectonic deformation, santanghu basin passed through four formation and evolution phases : ( 1 ) formation and evolution of basin ' s basement ; ( 2 ) formation and evolution of fault - fold to depression basin in permian ; ( 3 ) formation and evolution of depression basin in triassic - jurassic - cretaceous ; (

    依據塘湖盆地殘餘地序列、沉積體系、沉積充填特徵和原型盆地恢復,以及不同構造構造變形特徵綜合研究分析,認為塘湖盆地經歷了如四個發展演化階段:前二疊盆地基底發展演化階段;二疊斷陷-拗陷盆地發展演化階段; :疊-侏羅-白堊拗陷盆地發展演化階段;-四系新生代盆地發展演化階段。
  2. The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic

    盆地基底由前寒武結晶基底和古生代褶皺基底組成,盆地蓋則經歷了二疊裂谷盆地、?白堊坳陷盆地和山間盆地演化過程。盆地主要沉積了二疊統巨厚火山巖、淺成侵入巖和凝灰巖;中二疊統蘆草溝組暗色泥巖、泥灰巖、白雲質巖石以及條湖組巨厚火山巖、侵入巖;疊系雜色砂礫巖、砂巖及灰色泥巖(紅上灰) ;以及侏羅深灰、灰色砂礫巖、砂巖、泥巖夾煤
  3. Firstly, based on the basin prototype, the triassic and jurassic mudstone and coal, the main source rocks of the basin, did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly, because of the thrusting happened in late cenozoic, the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly. thirdly, the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow. as a result, the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas, but also developed simultaneously when the gas migration happened

    從盆地構造史研究角度認為庫車盆地天然氣主要來源於北部山前沖斷帶: 1受原型盆地構造格局制約,疊系侏羅系烴源巖發育最有利位置不是在拜城凹陷,而是在克依構造帶及其以北北部山前沖斷帶2晚以來逆沖推覆作用使得烴源巖提早進入高過成熟階段,並以產氣和凝析油為主3逆沖推覆作用所產生北傾逆斷控制天然氣自而上自北而南運移,位於運移路線上克依構造帶和秋里塔格構造帶東段與烴源巖排氣期匹配較好,從而使這些地區最富集天然氣。
  4. From the dongying formation ( ed ) to neogene, the shahejie formation was located in the late diagenetic stage a1 ~ a2 ; the oil and gas pools formed in a wide scale. at present the lower e2s3, with overmatured source rocks and low porosity reservoir rocks, gets into the late diagenetic stage b - c in the northern qibei sag where is not favorable for petroleum accumulation, but the others of the shahejie formation are locate still in the late diagenetic stage a1 - a2 and propitious to form oil and gas pools based on the diagenetic numerical modeling under the condition of overpressure, we build a multiple unit cubic equation model for porosity prediction, as the result of the application of qibei sag, the prediction error is less than 2 %, and the precision excess that of foreign same model

    歧北凹陷模擬結果表明,在沙河街組沉積末沙河街組段就進入晚成巖階段a _ 1期,油氣藏開始形成;在東營組沉積時期晚,沙河街組大部分地處于晚成巖階段a _ 1 a _ 2期,生、儲、蓋發育,是其主要成藏期;現今在歧北凹陷北部沙部進入晚成巖階段b c期,儲物性較差、不利於成藏,其他段仍處于晚成巖階段a _ 1 a _ 2期,有利於油氣藏形成。
  5. Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin - controlled faults, tanlu fault zone strike slip to develop the three nw - trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben. based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene. the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull - apart basin in cenozoic time. the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin - controlled faults in the different depresses in bohai basin. the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin

    根據中生界上侏羅統和白堊統地和控盆斷裂分佈分析,中生代晚期晚侏羅早白堊世郯廬斷裂帶左旋走滑平移導致郯廬斷裂帶以西自北向南發育了3個北西向斷塹系,即北部渤海斷塹系中部濟陽斷塹系和南部魯西南斷塹系。從區域資料綜合分析,渤海灣盆地基本格局是早以來新生代盆地格局。渤海灣盆地形態構造和沉積特徵及熱流值分佈表明該盆地在新生代為拉分盆地。
  6. Situated at the both e w sides of pamir, the s w tarim and tadjik basins have the similar evolution history of tectono sedimentary processes during cenozoic, i. e. steady subsidence with transgressive sequence in paleogene and speedy subsidence with continental molassetype sediments in strong compressive tectonic environment in neogene - quaternery. since neogene, for the effect of pamir and west kunlun s northward moving and thrusting, there is complicated tectonostructural deformation taking place in tadjik and sw tarim. neogene stratigraphic combination and later structural deformation of tadjik basin and southwestern tarim much resemble each other in terms of extent of transpressional processes. paleogene in tadjik basin is main oil - bearing sequence and many substantial oil - gas fields there have been found. so, it can be assured in comparison that there is oil - gas perspective also in southwestern tarim region

    受強烈擠壓快速沉降接受陸相磨拉石沉積。自新以來,受帕米爾西昆侖北移和隆升沖斷影響,塔西南和塔吉克盆地發生了復雜褶皺沖斷變形,其差異在於塔西南明顯地受走滑為主剪壓構造作用,而塔吉克盆地是受擠壓為主剪壓構造作用影響。塔西南和塔吉克盆地系巖相組合類似,後期構造變形也相似,塔吉克盆地系是該盆地主力油,已有許多油氣田發現,因此可以推斷塔西南也應該有良好油氣前景。
分享友人