陸緣沉積作用 的英文怎麼說

中文拼音 [liùyuánchénzuòyòng]
陸緣沉積作用 英文
epicontinental sedimentation
  • : 陸數詞(六的大寫) six (used for the numeral 六 on cheques, etc. to avoid mistakes or alterations)
  • : Ⅰ名詞1 (緣故) reason 2 (緣分) predestined relationship 3 (邊) edge; fringe; brink Ⅱ動詞(攀...
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • : Ⅰ動詞1 (使用) use; employ; apply 2 (多用於否定: 需要) need 3 (敬辭: 吃; 喝) eat; drink Ⅱ名...
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. 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

    在華南造山帶盆地分析和演化研究中,對揚子大東南邊從震旦紀到三疊紀環境,特點,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,被動大到前盆地華南造山帶格架。
  2. In the link party of qinling - qiliang - kunlun belt, the polyarc - basin systemic characteristic is discussed with strengthen and standout study on the detail relationship analysis between the arc - basin. the bayan har basin thought to be the preexistence of the songpan - garze belt, is a back - arc basin among a series of polyarc - basin systems behind the qiangtang - taniantawong front the arc beginning in the late paleozoic. the eastern margin started as the western passive continental margin of the yangtze block ( d - t2 ), then changed into a foreland basin related to the north china block and the qiangtang block during the middle to late triassic

    在秦祁昆侖結合部研究中,加強和突出了精細的島弧盆分析和造山關系的研究,探討了秦、祁、昆結合部多島弧盆特徵;通過巴顏喀拉地區特徵,體的空間展布和形態,面式物源供給方式,礦物成分和地球化學背景分析,其盆地屬性總體上反映出一個從過渡地殼-洋殼基礎上發育起來的周盆地的發展和演化過程。
  3. 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,建立了被動大盆地和相坳陷盆地的地層層序模式和層序聚煤模式,並對兩者聚煤了簡要對比。
  4. Source to sink : sedimentation in the continental margins

  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

    初步總結了被動大中典型底辟構造與天然氣水合物的成礦關系,認為被動內巨厚層、塑性物質與高壓流體、外側的火山活動及張裂,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。
分享友人