鼻周期 的英文怎麼說

中文拼音 [zhōu]
鼻周期 英文
nasal cycle
  • : 名詞1. (鼻子) nose 2. [書面語] (開創; 創始; 開端) start; origination; initiation
  • : Ⅰ名詞1 (圈子; 周圍) circumference; periphery; circuit 2 (星期) week 3 [電學] (周波的簡稱) c...
  • : 期名詞[書面語]1. (一周年) a full year; anniversary 2. (一整月) a full month
  1. The basin - formed mechanism, evolution model and petroliferous geological features of compresso - shear basins in the world are analyzed, by which six aspects of the features are summarized as follows : 1 ) in the compresso - shear process, the sedimentary speed of basin is high, forming thicker coarse - grained clastic rocks which normally shape good petroleum reservoir ; 2 ) the source rocks of basin tend to coming from the organic matter - enriched rocks formed in pre - compresso - shear stages, except that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in pre - compresso - shear stages, e4xcept that in intense compresso - shear process, deep water - semi deep water source rocks are possibly developed in frontal of deep depression ( fore deep ) of thrust belt ; 3 ) the en echelon folds ( including anticline and fault - nose structure ) are generally as good oil traps ; 4 ) the compresso - shear process is helpful to hydrocarbon accumulation ; 5 ) it may promote the maturity and hydrocarbon - generating process of organic matte, and 6 ) the thrust belts in the surrounding areas of compresso - shear basin are favorable are favorable domains for petroleum concentration

    摘要通過對世界上壓扭性盆地的成盆機制、演化模式和油氣地質特點分析,總結壓扭性盆地具有6個方面的石油地質特徵:壓扭作用間盆地的沉積速率較高,一般形成較厚的粗碎屑沉積,它們常構成很好的油氣儲集層:盆地的烴源巖往住來自於前壓扭砂成的富含有機質的巖石,但在強烈的壓扭作用間,在沖斷帶的前緣深坳陷(前淵)中有可能發育深水半深水相的烴源巖;壓扭(張扭)作用間形成的雁行式褶皺(包括背斜和斷等)往住是很好的油氣圈閉;壓扭作用易於成藏;壓扭作用可以促進有機質的成熟生烴作用;壓扭性盆地的邊沖斷帶是油氣賦存的有利部位。
  2. In a tidal cycle, waglan island is typically the first to experience the highlow tide while tsim bei tsui is generally the last

    在一個潮汐內,通常漲潮和退潮會首先在橫瀾島出現,而尖咀則比較遲。
  3. In a tidal cycle, waglan island is typically the first to experience the high low tide while tsim bei tsui is generally the last

    在一個潮汐內,通常漲潮和退潮會首先在橫瀾島出現,而尖咀則比較遲。
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