白堊紀的 的英文怎麼說

中文拼音 [báièjìde]
白堊紀的 英文
cretaceous
  • 白 : Ⅰ形容詞1 （似雪的顏色） white 2 （清楚; 明白; 弄明白） clear 3 （空的; 沒加他物的） pure; clear; ...
  • 堊 : Ⅰ名詞（白堊; 白土） chalkⅡ動詞[書面語] （用白堊塗飾） cover with chalk; chalk
  • 紀 : 紀名詞（姓氏） a surname
  • 的 : 4次方是 The fourth power of 2 is direction
  • 白堊紀 : chalk
  1. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山帶長期處于擠壓環境，伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝弧盆體系的遠距離效應使東秦嶺大別地區的外部擠壓消失，導致造山帶巖石圈迅速強烈拆沉伸展和減壓增溫熔融，從而形成大規模早白堊世花崗巖類和中酸性火山巖。
  2. The term is used at various localities in north africa, includes beds ranging from carboniferous to early cretaceous.

    在北非不同的地方使用這個名稱，包括從石炭紀到早白堊紀的地層。
  3. Cryptozoologists are especially proud of the catch in 1938 of a coelacanth, an archaic - looking species of fish that had been thought to have gone extinct in the cretaceous

    令未知生物學家尤其驕傲的是1938年捕捉到的腔棘魚， ?是一種樣貌古老的魚類，原先認為在白堊紀便已滅絕。
  4. The cretaceous extinction was like a terrible streak of bad luck lasting millions of years.

    白堊紀的生物絕滅，猶如一場持續千百萬年的可怕厄運。
  5. Only in the tropics were numerous late cretaceous groups extinguished during peaks in their evolution.

    只是熱帶地區才有大批晚白堊紀生物類群正值其演化的極盛時期突然消亡。
  6. The stippled area shows the distribution of a clean, permeable sandstone in the lower part of the lower cretaceous muddy formation.

    圖上畫點部分為下白堊紀馬迪組下部潔凈，滲透的砂巖分佈區域。
  7. Extreme climates events in the cretaceous and paleogene

    白堊紀至早第三紀的極端氣候事件
  8. The last dicynodont : an australian cretaceous relict

    白堊紀的最後的二齒獸[論文摘要] ！ ！
  9. Cretaceous period, 145 million years ago, was the age of the dinosaurs

    白堊紀期間， 145百萬年前，是恐的年。
  10. Climatological data from fossil pollen, leaves and wood indicate that the cretaceous forests of northern alaska consisted of a mixed canopy that included deciduous conifers with an understory of flowering plants, ferns and cycads

    由花粉、葉子和木材化石?集到的氣候資料顯示，阿拉斯加北部的白堊紀森林有混合型林冠，包括了落葉針葉林以及林下的開花植物、蕨類和蘇鐵。
  11. The cretaceous is named after the large amounts of chalk ( fossilized plankton ) found in rocks of the period

    白堊紀以這個時代的地層主要為白堊沉積而得名。
  12. The hanging wall of sag extended in southeast direction, with the tulage fault being the boundary fault. yinggete - bagemaode metamorphic core complex developed adjacent to northwest of chagan sag, which evolved from late jurassic to cretaceous with three - layer construction style. the kinematics mechanism of metamorphic core complex and chagan sag is a simple shear model, chagan sag extended and faulted as the metamorphic core complex rised

    在查干凹陷西北側發育英格特?巴格毛德變質核雜巖帶，可能具有三層結構模式，其形成與演化時代為晚侏羅世末?白堊紀；該變質核雜巖與查干凹陷的運動學機制為統一的簡單剪切模式；在變質核雜巖隆升的同時，查干凹陷發生伸展斷陷。
  13. Yanqi basin is stituated between tarim basin and tarpan - harmi basin. its petrolenm system underwent the formation and destruction during jurassic - cretaceous, the activation and reconstruction during tertiary - quaternary

    焉耆盆地位於塔里木盆地和吐哈盆地之間，其含油氣系統經歷了侏羅紀-白堊紀的形成與破壞階段和第三紀-第四紀的活化與再建階段。
  14. 4. combined with the analysis of the hydrocarbon - generation history, hydrocarbon maturity, fluid inclusions, authigenic illites isotopes chronology and trap forming history, it affirms that jurassic reservoirs formed in three phases : the first in the late jurassic, which was the primary pool - forming phase, the second in the telophase of jurassic to cretaceous, which was the adjusting - destroying phase, the third in tertiary, which was the secondary phase

    4 、採用烴源巖生烴史、油氣成熟度、流體包裹體、儲層自生伊利石同位素年代學和圈閉演化史綜合方法，確認焉耆盆地侏羅系油氣藏具有三期成藏的特點，第一期發生在侏羅紀晚期，是盆地的主要成藏期，第二期為侏羅紀末至白堊紀的油氣藏破壞、調整和再分配期，第三期發生在第三紀，是盆地的次要成藏期。
  15. 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

    盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖；三疊系雜色砂礫巖、砂巖及灰色泥巖（下紅上灰） ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。
  16. The results indicate that most of the lithologic oil accumulation of the three main depressions in erlian basin eventually formed in early to mid cretaceous, and compared with most structural oil accumulation in the basin the lithologic ones represent the characteristic of relatively earlier formation period

    研究表明，二連盆地3大主力凹陷巖性油藏的成藏期多在白堊紀的早、中期，相對於二連盆地構造油藏的形成期具有明顯的早期成藏的特徵。
  17. It is suggested that " maodun intrusion " may be an pre - cretaceous intrusion, that the early cretaceous " hantamiao secondary depression " divided by the predecessor may not exist. maonan fault might activited strongly during pre - cretaceous

    「毛敦侵入體」可能為一前白堊紀的侵入體，前人所劃分的早白堊世「罕塔廟次凹」可能不存在，毛南斷層可能為一前白堊紀強烈活動的老構造。
  18. Alvarez did well in pro viding evidence for a cretacious / tertiary impact but left much to be desired when considering its results

    阿爾瓦雷茨很好地為三疊紀白堊紀的大碰撞提出了證據，但當考慮它的結果時，卻留下了很多要思考的問題。
  19. This paper analyzes the sedimentation and the occurrence of the strata in wuxia area and suggests that wuxia area underwent the development of foreland basin of early permian, the overthrust nappe of late permian, the strong structural uplift of late triassic, the weak structural activity of late jurassic and the structural shape of cretaceous followed by finally forming the configuration nowadays

    在對烏夏地區地層的沉積特徵和產狀分析后發現，烏夏地區經歷了早二疊世的前陸盆地發育階段、二疊紀末的逆掩推覆，三疊紀末的構造強烈隆升、侏羅紀末期的構造微弱活動、至白堊紀的構造定形等多個階段的演化而形成了現今的面貌。
  20. During his journey the incredible diversity of life in the early cretaceous period is revealed

    從它的旅程當中還可看到種種早期白堊紀的生物。
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