margin of continental shelf 中文意思是什麼

margin of continental shelf 解釋
大陸架邊緣
  • margin : n 1 邊緣;邊緣部分;范圍,限界;【軍事】圖廓。2 (版心外)空白;欄外,欄外註解。3 【商業】原價和...
  • of : OF =Old French 古法語。
  • continental : adj 1 大陸的;大陸性的。2 〈C 〉 歐洲大陸的,〈C 〉〈美國〉(獨立戰爭時)美洲殖民地的。n 1 歐洲大...
  • shelf : n (pl shelves )1 擱架;擱料架;擱板。2 沙洲;暗礁。3 格;層。4 【礦物】平層;錫沙礦基巖;【航海...
  1. The carbonate source rocks of middle - upper ordovician in tarim basin are widely distributed in different sedimentary environments at the same period such as platform margin slope, platform inner sag, continental shelf, abyssal basin, etc

    摘要塔里水盆地中上奧陶統碳酸鹽巖烴源巖在同一時期不同的沉積環境(臺緣斜坡、臺地內凹陷、陸棚、深海盆地等)中均有發育。
  2. The juridical continental shelf of a coastal or island nation consists of the seabed and subsoil of the submarine areas that extend beyond its territorial sea to the outer edge of the continental margin, or to a distance of 200 nautical miles from the baseline used to measure the territorial sea where the continental margin does not extend to that distance

    書上的翻譯:沿海國或者島國法律上的大陸架包括延伸到其領海以外直到大陸邊緣外部界限的海底區域的海床和底土;如果從測算領海寬度的基線起到大陸邊緣的距離不到200海里,則應擴展到200海里的距離。
  3. According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime - mud reef in platform margin, platform inner sag, deep - water flat slope or continental shelf, abyssal basin, the lime - mud reef type is distributed in platform margin of upper ordovician, the remained three types are widely distributed in cambrian - ordovician system

    根據沉積相帶與沉積環境的不同,可將烴源巖劃分為在不同沉積環境中的4種類型烴源巖;臺地邊緣灰泥丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與陸棚型烴源巖、深海盆地型烴源巖。
  4. The lower paleozoic continent marginal sedimentary strata in the north kunlun massif are sinian - cambrian alajiaoyi group and ordovician pishigaisayi formation. the former is composed of high maturity flysch deposit, the later consist of continental shelf deposit such as carbonate and slate and sandstone. these rocks implies that they might form at passive continental margin

    與其曼于特蛇綠巖相關的早古生代邊緣沉積巖在昆北地塊上為震旦?寒武系阿拉叫依巖群、奧陶系皮什蓋薩依巖組,前者為一套成熟度較高的陸源碎屑復理石沉積,後者為碳酸鹽巖和含碳板巖砂巖等陸棚沉積,顯示其具被動陸緣性質。
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