造山運動前的 的英文怎麼說

中文拼音 [zàoshānyùndòngqiánde]
造山運動前的 英文
preorogenic
  • : Ⅰ動詞1 (做; 製作) make; build; create; produce 2 (假編) cook up; fabricate; concoct 3 [書面語...
  • : 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...
  • : 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...
  • : Ⅰ名詞1 (在正面的) front 2 (次序在先的) first; top 3 (過去的; 較早的) ago; before; preceding...
  • : 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. That mountainous city road is the public exhibition of a mountainous country city, affecting the whole image of the city, but the necessery gardenlization streets sight design is a means to increase city image. however, city that front with several design how to beautify the sport for the characteristic with the estheticism, to mountainous city, the road ' s gardenlization streets sight design results in ecology problem, and more roads are not widespread thought of

    地城市道路是地城市公共展廊,它影響著城市整體形象,而必要園林化街景設計是提高城市形象手段。然而,當以幾何設計和唯美主義為特徵城市美化,對地城市園林化街景設計,成生態環境問題,而更多街景設計未被普遍重視。
  2. The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution. the basins located in the southern margin of the yangtze plate, in the basin dynamic computer simulation, is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt

    在沉積盆地分析方面,基本查明揚子板塊東南邊緣早古生代被大陸邊緣沉積特徵及沉積構演化,同時用反剝法技術對揚子板塊東南大陸邊緣沉積盆地形成,演化沉降力學進行探討,用計算機模擬方法,定量力沉積學對揚子東南邊緣奧陶紀到志留紀陸地進行計算機模擬分析,探索並建立這個古老陸盆定量參數和態定量模擬。
  3. 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個有利勘探區帶,它們是:庫車陸沖斷帶古近系、新近系膏鹽巖、膏泥巖之下完整背斜圈閉;準南陸沖斷帶第二、第三排構帶;川西北部及南部燕期古隆起、川中平緩褶皺構帶以及深坳陷內部非常規天然氣;柴北緣冷湖南八仙構帶。
  4. 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

    數干萬年地質史上最年輕大規模,隆起了雄侵喜瑪拉雅、網底斯、昆侖、唐古拉起了「世界屋脊」 。
  5. The yanshan - liaoning area is called as the " cradle of geology ". it is the first time that the geologist, wen wenghao, has put forward the " yanshan movement " before 70 years. from then on the yanshan - liaoning area had been paying attention by the geologists all over the word because it lies in the particular tectonic background, has the complex structural features, structural units, and the geological history of evolution, particularly large - scale, multi - phrase tectonic movement and magmatic activity took place in the short geological time

    燕遼地區素有地質「搖籃」之稱,自翁文灝在70餘年提出yenshanmovement (燕)以來,它以其獨特大地構位置、復雜特徵、組成及其演化過程,特別是該地區在很短時間間隔內發生了大規模、多幕式構?巖漿活,更引起世界地學界極大關注。
  6. It is very important that the understanding of regional metallogenic rules should be emphasized and the thinking of exploration and research opened up. in this thesis, mainly metallogenic types, tectonic setting, space - time distributions and the ore - controlling and metallogenic conditions for copper ore deposits in gansu province are studied on based inducing past formation which basic theories and methods of the modern geology, mineral deposits and related learning are applied and a serious of formation synthesized throughout depending on guide of regional. - metallogenic theories. a rule of development, enrichment and regional metallogeny would be preliminary summaries in terms of analyzing mineral prospecting for gansu ' s copper, gold and polymetallic minerals, and the relation between the indosinian - yanshan structural - magmatic activities is studied and exploration prospect and positions analyzed as well as a new countermeasure and thinking about research for minerals in this area be suggested

    本論文在總結、分析人成果資料基礎上,以區域成礦學理論為指導,用現代地質學、礦床學及相關專業、學科基本理論與方法,綜合多種成礦信息,對甘肅省銅礦主要成礦類型及其成礦地質構背景、時空分佈特徵與主要控(成)礦條件進行了研究;從礦產勘查角度,初步總結了甘肅銅、金及多金屬礦產發育、富集與區域成礦規律;探討了印支-燕期構-巖漿活與大型-超大型銅礦床形成關系;研究分析了甘肅銅礦資源勘查景與找礦方向,提出了該區礦產勘查研究新思路。
  7. The tectonic motion is very intense in front belt of north tianshan mountain, drape fault and so on very develop, and there occurred many times destruct earthquakes

    摘要北天地帶是構十分強烈地區,褶皺斷裂等構現象十分發育,這里曾發生過多次中強破壞性地震。
  8. Under the effect of regional tectonics, there develop many raws drape anticline and active fault in the front of mountain, and they have especial motion fashion

    由於受區域構長期作用影響,在北天地區逐步發育形成了多排褶皺背斜及活斷裂,且方式具有獨特性。
  9. 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

    ,是中國五嶽之首,古稱「岱宗」 ,形成於25億年,是第一次興起它位於東省中部,華北大平原東側,京滬鐵路中段。
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