起堊 的英文怎麼說

中文拼音 [è]
起堊 英文
chalking
  • : 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...
  • : Ⅰ名詞(白堊; 白土) chalkⅡ動詞[書面語] (用白堊塗飾) cover with chalk; chalk
  1. Moisture evaporating from the chalk of tsochen s moon world badlands in the warmth of the early morning sun shrouds the hills in mist, like a scene from an ink - wash painting. but to enjoy this sight you have to rise early, and have luck with the weather

    月世界白土中的水分受日出而蒸發,水汽蒸蒙的層疊山巒如同一幅氣勢磅礴的水墨畫,不過欲賞此美景必須個大早,有好天氣配合。
  2. Recently, a series of the feathered dinosaurs have been found from the jehol biota of western liaoning, northeast china, which give extremely strong evidences of the theropod hypothesis of bird origin and of the cursorial hypothesis of the avian flight origin. but the origin and early evolution of feathers have still been unanswered. in late 2000, a well - preserved specimen of dromaeosaurids was excavated from the early cretaceous jiufotang formation of shangheshou, suburb of chaoyang city, western liaoning

    2000年,遼西朝陽市上河首早白世九佛堂組地層中,發現了一件保存完好的長有羽毛的奔龍類化石,這是繼北票四合屯、朝陽下三家子、凌源大王杖子之後長羽毛奔龍化石在遼西的又一次發現,為解決奔龍類的系統關系、羽毛的源及早期演化提供了重要的實物資料。
  3. Erlian basin is a rift lacustrine basin developed on the hercynian geosyncline folded base in early cretaceous, is featured by simple sedimentary feature, depositional cycle, small lacustrine transgressive, dry climate, salinization lacustrine water and multi - and - near sources

    摘要二連盆地是在海西期地槽褶皺基底上發育來的早白世斷陷湖泊群,具有湖盆湖浸規模較小、氣候條件乾燥、湖水咸化、沉積旋迴單一,多物源、近物源和粗碎屑等沉積特徵,以及發育巖性地層油氣藏為主的油氣分佈特點。
  4. The flare of the gas - jets, the open trunks, suggestive of travel and display, the scattered contents of the make - up box - rouge, pearl powder, whiting, burnt cork, india ink, pencils for the eyelids, wigs, scissors, looking - glasses, drapery - in short, all the nameless paraphernalia of disguise, have a remarkable atmosphere of their own

    耀眼的煤氣燈,打開的箱子令人想旅行和排場,散亂的化妝用品-胭脂珍珠粉白粉軟木炭墨汁眼瞼筆假發剪刀鏡子戲裝-總之,各種叫不上名來的化妝用的行頭,應有盡有,各有自己獨特的氣息。
  5. The texas state capital sity straddles the line between two geologic provinces - to the west is the uplifted plateau of cretaceous limestones and exposed precambrian llano uplift, while the lowland bladk prairie country stretches eastward for miles

    西部是白質的石灰石突的高處地帶和暴露的precambrian llano突出處,而低處的black prairie直向東部擴展數里。
  6. Being primarily controlled by northwest faults, cretaceous of jiyang depression contained several isolated basins, and lake levels of these isolated basins were instable, but on the whole, shore and shallow lake sub - facies is in the majority

    北西向斷層的活動對沉積到主要的控製作用,在其控制下,白紀濟陽坳陷為一相互分割的山間盆地,湖盆范圍時大時小,湖水深度不斷變化,總體湖水較淺,主要發育濱淺湖亞相。
  7. During the yanshanian phrase, the area is in the condition of contractional background, with multi - staged tectonic reversion. 5. through studying the origin of volcanic rocks and the characteristics of magma evolution, it concludes that there exist 3 originated areas of magma - from mantle, crust, and mantle - crust exchange. the basic magma of nandaling volcanic rocks of early jurassic is derived from upper mantle ; the magma of tiaojishan volcanic rocks of mid jurassic is formed in the contractional tectonic setting, and derived from the transition zone of crust and mantle interaction ; the acid magma of l

    5 、通過巖石化學、微量元素、稀土元素的研究,探討了不同級別節律的火山巖成因、巖漿演化等特徵,認為本區燕山期火山巖有三個巖漿源區,即地幔源、地殼源和殼幔混源,早侏羅世的南大嶺旋迴的基性巖漿,源於上地幔;中侏羅世髫髻山旋迴火山巖是在相對擠壓環境中,巖漿源於殼幔過渡帶;晚侏羅世無負eu異常的酸性巖漿來源於下地殼的古老結晶基底的局部熔融,有負eu異常的酸性巖漿來源於上地殼的局部熔融;早白世火山巖基性巖漿源於上地幔,中性巖漿源於下地殼底部的殼幔過渡帶。
  8. The residue formed by partial melting of thickened crust due to anomalous heat supply by mantle superwelling at early cretaceous is possibly easy to detach from the crust because of its high density, leading to the remove of mountain root and large scale uplift of the orogen

    早白世地幔超柱事件熱擾動所引的加厚地殼部分熔融后的殘留體可能由於比重較大而拆離進入地幔,從而發生去山根作用和造山帶的大面積隆
  9. He origin of early cretaceous volcanic rocks of ixian formation and crust - mantle interaction n west liaoning province, eastern china

    遼西早白世義縣組火山巖的源及殼幔相互作用
  10. Modern birds are the only group of mesozoic birds to have survived after the k / t extinction event, and recent ornithurine discoveries lend further support to the cenozoic origin of the modern avian groups

    現生鳥類是白紀與第三紀之交絕滅事件發生之後的倖存類群,近來今鳥類的新發現也進一步支持了現生鳥類源於新生代的推論。
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