造山運動的 的英文怎麼說

中文拼音 [zàoshānyùndòngde]
造山運動的 英文
orogenic
  • 造 : Ⅰ動詞1 （做; 製作） make; build; create; produce 2 （假編） cook up; fabricate; concoct 3 [書面語...
  • 山 : 名詞1 （地面形成的高聳的部分） hill; mountain 2 （形狀像山的東西） anything resembling a mountain...
  • 運 : Ⅰ動詞1 （物體位置不斷變化） move; revolve 2 （搬運; 運輸） carry; transport 3 （運用） use; wield...
  • 的 : 4次方是 The fourth power of 2 is direction
  • 運動 : 運動[舊時用語] arrange things or get things done through pull
  1. Many ultrabasic bodies in the orogenic association occur along strike faults, which gives a simulated concordant relationship.

    與造山運動共生的許多超基性巖體沿著走向斷層出露，表現出假的整合關系。
  2. K - ar age of an illite from alteration rock in the contact zone around lianhuashan porphyry is 38. 6ma. with referencing to the main metallogenic period of yulong copper metallogenic zone and of ailaoshan gold metallogenic zone, it is suggested that the time of formation of deposits in the district studied is probably in a period of time from 38. 6ma at earliest to 20ma at latest. this time is equivalent to the origination time of two important tectonic events, i. e., lanping movement and the turning point when ailaoshan - red river fault turned from sinisteral into dextral

    獲得了蓮花山巖體周圍接觸帶蝕變巖中伊利石k - ar年齡38 . 6ma ，參考玉龍銅礦帶和哀牢山金礦帶的主要成礦期（分別為30ma左右及26ma ） ，釐定本礦集區成礦年齡下限為38 . 6ma ，上限為20ma ，與兩次重要的構造事件?蘭坪運動的起始時間及哀牢山?紅河斷裂由左旋轉為右旋的時間相當。
  3. The period was one of general emergence and orogeny.

    這個時期是全面的上升和造山運動。
  4. 2. 38. 6ma and 36. 7ma isotopic ages of quartz - monzonite - porphyry in lianhuashan and alkaline porphyry in zhuopan have respectively been obtained. those results are consistent with the ages of the porphyries in both lanping - shimao basin and changdu basin related igneous rocks, representing the first episode ( lanping movement ) of tectonics - magmatism - metallogenic event during the himalayan movement

    獲得了蓮花山石英二長斑巖及卓潘堿性斑巖的ar - ar年齡，分別為38 . 6ma與36 . 7ma ，與整個蘭坪?思茅盆地與昌都盆地及兩側的斑巖與相關火山巖一致，代表喜馬拉雅運動第一幕（蘭坪運動）的重要構造?巖漿?成礦事件。
  5. Occurred in the neozoic, the strong himalayan movement made the first order and the second order structure units uplift to form maintains in the basin, which are unfav orable to preserve oil and gas

    新生代發生的強烈的喜山運動，促使盆地內部各一、二級正向構造單元進一步沖斷上隆、甚至生長為盆內山脈，對古油氣藏保存不利。
  6. The study results on hydrocarbon preserving conditions have suggest ed that influenced by latter tectonic movements, especially by the yanshan ~ himalayan tectonic movement, obviously different hydrocarbon preserving conditions occur between the eastern and the western parts bounded by the qiyue mountain. the whole lower paleozoic hydrocarbon enclosing and preserving conditions for the shizhu synclinorium - fangdoushan antici inorium to the west of qiyueshan mountain have the advantage over those of the qiyueshan antici inorium - lichuan synclinorium to the east of qiyue mountain

    通過油氣保存條件的研究認為：受後期構造運動的影響，尤其是燕山期?喜山期構造運動的影響，造成區內以齊岳山為界東西油氣保存條件存在明顯差異，齊岳山以西的石柱復向斜?方斗山復背斜下古生界油氣整體封存條件明顯優于齊岳山以東的齊岳山復背斜?利川復向斜。
  7. According to these results combined with exploration practice, foot favorable exploration zones are selected, these are the integrated anticline traps below the tertiary gypsum halite, gypsum mudstone in kuqa foreland thrust belts, the second and the third row structural bells in southern junggar foreland thrust belt, the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin, the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin, and the cold take and nanbaxian structural belt in northern margin of qaidam basin

    依據理論分析及勘探實踐，優選出4個有利的勘探區帶，它們是：庫車前陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下的完整背斜圈閉；準南前陸沖斷帶第二、第三排構造帶；川西北部及南部燕山運動期古隆起、川中平緩褶皺構造帶以及深坳陷內部的非常規天然氣；柴北緣冷湖南八仙構造帶。
  8. There existed several strong reformation of late - yanshan movement and himalaya movement the generation, development, disappearance and reformation are tightly related to tarim block, tianshan belt and tethyan tectonic zone, especially tianshan belt, which makes the great difference between present and original basin

    該盆地形成后經歷了燕山晚期和喜山期構造運動的多期強烈改造；其產生、發展和消亡以及改造與塔里木地塊、天山構造帶、特提斯構造域的演化息息相關。其中尤以天山構造帶的活動影響最大，從而造就盆地今古面貌差異巨大。
  9. According to the analysis of the structure deformation variant direction the structure superposition during late period, and the tectonic stress field and deformation variant field, the cover extended nearly sn direction in early stage ( d - c ), maybe changed the direction in pernian ( especial the late permian ), and developed some new half - graben along sn direction except the succession activity at great fault zone. the direction of compression deformation variant, however, was nearly sn direction in indo - chinese epoch, ne - sw direction in early yanshan movement epoch, nne - ssw direction in late yanshan movement epoch, and transformed from ew to sn direction in himalayan movement epoch

    根據不同構造層中變形方向及後期構造疊加的分析，對本區的構造應力場及變形場進行了探討，本區蓋層早期階段（ d - c ）為近南北向的伸展拉張，二疊紀（特別是晚二疊世）的伸展方向可能發生了改變，除在各斷裂帶繼承性活動外，沿南北方向又新生了一些半地塹。而在擠壓變形時，印支期主要為近南北向擠壓，燕山早期為nw - se向擠壓，燕山晚期為nne - ssw向擠壓，而喜山運動可能經歷了從ew向向sn向方向擠壓的轉變。
  10. The tectonic plate motions, especially at the convergent edge of the lithospheric plate, such as building mountain, earthquake eruption, island - arc and trough development, and so on, which are close related on the human inhabiting environment

    板塊構造運動，特別是巖石圈板塊匯聚地帶的構造運動? ?造山運動、地震爆發和島弧海溝的形成等，這些與人類生存環境息息相關。
  11. The two worlds, nocturne and its oversized moon prometheus, circle each other in an erratic orbit, causing massive tectonic activity across the thin crust of nocturne

    那克土恩和它那大於一般的衛星普羅米修斯相互的以飄忽不定的方式旋繞，這也造成了星球上極其不正常的巖層活動和火山運動。
  12. The continental orogenesis is characterized with the following features, such as sudden start, global synchronicity and horizontal movement, occurring mainly in the upper part of the crust and weakening with depth, and so on

    摘要大陸皺造山運動具有突發性、全球同步性，以水平運動為主，主要表現在地殼上部且具有上強下弱等特徵，除水平運動一項外，與基於地幔對流的板塊構造理論缺少共同之處。
  13. Surviving the mountain building process while in the mountains is precarious, and not advised

    想要躲過造山運動地質災害的話，待在山裡是不可靠的，而且我們不建議那麼做。
  14. The qiongzhong granite should have been formed at orogenic relaxing stage after the peak of indosinian orogeny, and the danxian granite were formed at the latest orogenic phase

    瓊中巖基可能形成於「印支期」碰撞造山運動峰期后的鬆弛階段，而儋縣巖基則可能形成於造山運動的結束階段。
  15. Tens of millions of years ago, as a result of massive orogenic movement, the spectacular himalayas, the kangdese, kunlun and tanggula mountains rose to form the roof of the world

    數干萬年前地質史上最年輕的大規模造山運動，隆起了雄侵的喜瑪拉雅山、網底斯山、昆侖山、唐古拉山，造起了「世界屋脊」 。
  16. Basin system is the united area of the deposition space and the denudation area. the evolution of the basin system can mirror the process of the related erogenic movement. the disintegration of a basin system indicates the end of one time of erogenic movement

    沉積盆地系統是堆積空間與蝕源區的統一，盆地系統的演化反映出造山運動的歷程，一個盆地系統的瓦解是一次造山運動的完成，同時又形成了新的盆地系統。
  17. Therefore the flexural stress covers a large percentage of the total stress field. the study of the flexural stress field of the continental lithoshpere in western china will contribute a lot to the understanding of the tectonic evolution of continental lithosphere and the global plate tectonics

    研究中國西部大陸巖石圈的撓曲應力場對于了解該區總應力場的性質、研究板內造山運動和青藏高原隆升以及地球動力學都具有非常重要的意義，有助於理解構造運動的動力機制和大陸巖石圈的運動特徵。
  18. The mountain was formed 2, 500 million years ago with the earth s primeval orogenic movement. located in the central part of shandong province, and in the east of north china plain, mount tai range stretches eastwards for more than 200 kilometres along south bank of the yellow river

    泰山，是中國五嶽之首，古稱「岱宗」 ，形成於25億年前，是第一次造山運動興起的大山它位於山東省中部，華北大平原東側，京滬鐵路中段。
  19. This paper reveals the collision energy of a celestial body with the earth could induce a sufficient change of rotating speed of the earth to make the folding orogenesis, and briefly explains its mechanics, and therefore offers a brandnew perspective for researching continental orogenesis

    揭示了星地碰撞可以為大陸造山運動提供足夠強大的突發性動力來源，並簡要闡明了其作用機制，可以解決地質力學所遇到的力源不足和被海水運動取代的兩大難題，從而為大陸構造研究開辟了一個新境界。
  20. 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的地質力學理論，對之所做的定性解釋頗為合理，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的動力來源，力量強度太小，不足以引發強大的褶皺造山運動，且有被海水運動取代的難題。
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