被動大陸邊 的英文怎麼說

中文拼音 [bèidòngliùbiān]
被動大陸邊 英文
passive margins
  • : Ⅰ名詞1 (被子) quilt 2 (姓氏) a surname Ⅱ動詞[書面語]1 (復蓋) cover; spread 2 (遭受) suffe...
  • : 陸數詞(六的大寫) six (used for the numeral 六 on cheques, etc. to avoid mistakes or alterations)
  • : 邊Ⅰ名詞1 (幾何圖形上夾成角的直線或圍成多邊形的線段) side; section 2 (邊緣) edge; margin; oute...
  • 被動 : passive; unactive; passivity
  1. 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緣早古生代被動大陸邊緣沉積特徵及沉積構造演化,同時運用反剝法技術對揚子板塊東南緣沉積盆地形成,演化的構造沉降力學進行探討,運用計算機模擬方法,定量力沉積學對揚子東南緣奧陶紀到志留紀前地進行計算機模擬分析,探索並建立這個古老造山帶前盆定量參數和態定量模擬。
  2. In a study on a sedimentary basin analysis of the huanan orogenic belt, the sedimentary basin character and evolution in the southeastern passive continental margin of the yangtze plate is investigated with elaborate sedimentary environments and sedimentary character from the sinian to the triassic, and then the sedimentation sketch of this belt is established especially to be from rift, passive continental margin into foreland basin in the early paleozoic on the yangtze plate

    在華南造山帶沉積盆地分析和演化研究中,對揚子東南緣從震旦紀到三疊紀沉積環境,沉積作用特點,沉積盆地性質和演化進行研究,特別是建立了中國南方揚子板塊早古生代從裂谷,被動大陸邊緣到前盆地華南造山帶沉積作用格架。
  3. Continental margins of so-called "passive" types are strongly coupled to any events at ridge crests.

    所謂「」型的緣與洋脊任何變事件有很關系。
  4. Abstract : in the light of sequence stratigraphic research work on permain coal - accumulating basins in south china and jurassic ordos coal - accumulating basin in north china, the sequence stratigraphic model and coal - accumulating model of passive continental margin and continental down warping basin were established, the comparison between both settings was also briefly conducted

    文摘:運用層序地層學原理,對華南二疊紀含煤盆地和侏羅紀鄂爾多斯含煤盆地進行研究,建立了被動大陸邊緣盆地和相坳陷盆地的地層層序沉積模式和層序聚煤模式,並對兩者聚煤作用作了簡要對比。
  5. The relationships between the accumulation of gas hydrates and the typical diapirs in passive continental margin are summarized in primary in this paper which suggest that the factors in passive continental margin including the thick sediment layers, plastic substance, high pressure fluid, outboard volcanic activities and the process of stretch - rupture provide favorable conditions for the formation of the diapirs which can form advantageous environment for gas hydrates coming into being

    初步總結了被動大陸邊緣中典型底辟構造與天然氣水合物的成礦關系,認為緣內巨厚沉積層、塑性物質與高壓流體、緣外側的火山活及張裂作用,為底辟構造發育提供了條件,形成了水合物成礦的有利空間。
  6. The geochemical examination of the sandstones and mudstones from the xikang group has led us to conclude that the debris are derived mostly from the surficial rocks and their overlying deposits on the xikang - yunnan ancient land, and tectonic settings display the transition from the passive continental margin to active continental margin and finally to archipelago

    通過對西康群砂、泥巖地球化學組成特徵研究,認為其物源來自康滇古表殼巖及其上覆的蓋層沉積,地構造屬性為被動大陸邊緣到活緣再到多島弧的轉化。
  7. On the basis of analysis on the characteristics of structural evolution, the growth of the source rocks is analyzed. in the period of mesozoic - palaeozoic, caledonian events and the evolution of hercynian - early indo - chinese cycle are experienced in two - phase marine passive continental margin and craton basin in the lower and middle yangtze region, by which stable enormous thick mesozoic - palaeozoic deposites are induced, six sets of source rocks are produced, it has a strong capacity of hydrocarbon generation

    摘要通過構造演化特徵分析了海相烴源巖的發育,中、下揚子區中古生代經歷了加里東和海西早印支旋迴兩個階段的海相被動大陸邊緣和克拉通盆地演化,形成了巖性穩定的巨厚中古生界,發育了6套烴源巖,具有較強的生烴能力。
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