有小褶的 的英文怎麼說

中文拼音 [yǒuxiǎode]
有小褶的 英文
wavelet
  • : 有副詞[書面語] (表示整數之外再加零數): 30 有 5 thirty-five; 10 有 5年 fifteen years
  • : Ⅰ形容詞1 (體積、面積、數量、強度等不大) small; little; petty; minor 2 (年紀小的; 年幼的) youn...
  • : 名詞(褶子) pleat; crease; fold; wrinkle
  • : 4次方是 The fourth power of 2 is direction
  1. 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皺基底上發育起來早白堊世斷陷湖泊群,具湖盆湖浸規模較、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油氣分佈特點。
  2. According to the spread of nappe and relation between the nappe and depression, oblique - thrust fault zone was divided into three parts in this paper : sertengshan, lvliangshan and xitieshan. ( 3 ) according to macroscopic characteristics of fault zone, cleavage characters of fault zone, drag folds, the reverse " s " fold in the footwall, positive flower structures and small left strike - slip fault, the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section, left - slip fault in plane and the strike - slip displacement increasing from the west to the east

    ( 3 )根據斷裂斷裂帶宏觀特徵、斷層帶劈理特徵、斷裂帶附近牽引皺和斷層下盤平面反「 s 」型皺以及斷層上盤剖面正花狀構造和平面左行型平移斷層,認為賽什騰-錫鐵山斷裂帶運動學主要表現為剖面上逆沖、平面上左行走滑特點,並且走滑量具自西向東增大之勢。
  3. The cbm industrial production region lies in transition zone which is one part of a single continent in u. s. a., but a compound continent that is made up of some small platform, landmass and fold belt in china

    我國是一些型地臺、地塊及其間皺帶鑲嵌起來復合大陸,煤層氣勘探利區位於地臺內部。
  4. Two hours after her departure, i was still sitting on the bed she had just left, staring at the pillow which bore the imprint of her head, and wondering what should become of me, torn as i was between love and jealousy

    她走了已兩個時了,我還是坐在她適才離開床上,凝視著床上枕頭,上面還留著她頭形,一面考慮著在我愛情和嫉妒之間我將變成什麼樣子。
  5. Nw compressive structures are developed in indosinian epoch in which folds are predominant and companied with some small thrusts. nearly ns or nnw compressive structures are developed at the end of yanshan epoch in which it is mainly overthrusted structures and closed folded structures. large gentle anticlines and synclines are developed from the end of mesozoic to early tertiary, and antithetic sagging structures are developed in mesozoic

    研究發現,本區印支期發育了以皺為主、局部伴型逆斷層北西向壓性構造,燕山末期(中生代末期)發育了以逆掩構造和緊閉皺構造為主近南北向或北北西向壓性構造,中生代末到第三紀早期發育了以寬緩為特徵大型背斜向斜構造,以及中生界內部逆牽引構造。
  6. There were more or less macrophage and mast cells in the lamina porpria connective tissue in trionyx ' s digestive tract. no microfold cells and lymphatic nodule were found in its digestive tract, which was different from mammal and avian

    鱉消化道粘膜結締組織中分佈數量不一巨噬細胞和肥大細胞,但與哺乳類和鳥類不同,鱉消化道未出現微皺細胞( microfoldcell , m細胞) ,未見淋巴結形戍。
  7. Near the studied area, the fossil microtine show a sequence from the early pleistocene to the mid - late pleistocene : allophaiomys ( qi ) ? redromys ( q ) ? icrotus ( q2 - i ) - on their molars, the 5th dentine isthmus is5 show a closed trend from broad to narrow and made the salient angle tend to gradual increase. in the area, the 6th dentine isthmus is6 of the microtus show a trend from broad to narrow gradually

    在研究區及其附近,更新世以來,田鼠類演替順序為: allophaiomys ? ? predromys ? ? microtus ,其第5齒峽is5相應由寬變窄,趨于封閉,使封閉角趨于增多;研究區內microtusoeconomus第6齒峽is6逐步變趨勢。
  8. The geomechanics based on the change of rotating speed of the earth could answer a large part of the above mentioned questions, but the power which it depends on offered by the expansion or contract of the earth and tides et al is too weak to serve as the energy to change the rotating speed of the earth, so it is also difficult to explain them quantitatively

    基於地球自轉速度變化地質力學理論,對之所做定性解釋頗為合理,但因其只靠地球收縮及潮汐引力等緩變力作為引起地球自轉速度變化動力來源,力量強度太,不足以引發強大皺造山運動,且被海水運動取代難題。
  9. Effect of structure on cbm formation and destruction reflects in three aspects : geological developing history, fold and fracture. region where valid depth is smaller than 200m has no exploration value

    構造對煤層氣藏形成和破壞主要表現在地質發展史、皺、斷裂三個方面,其中上覆地層效厚度於200m地區不具備勘探價值。
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