陸棚邊緣 的英文怎麼說

中文拼音 [liùpéngbiānyuán]
陸棚邊緣 英文
shelf-edge
  • : 陸數詞(六的大寫) six (used for the numeral 六 on cheques, etc. to avoid mistakes or alterations)
  • : 名詞1 (用竹木等搭成的遮蔽太陽或風雨的設備) canopy or awning of reed mats etc : 茶棚 tea booth; ...
  • : 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...
  • : Ⅰ名詞1 (緣故) reason 2 (緣分) predestined relationship 3 (邊) edge; fringe; brink Ⅱ動詞(攀...
  • 邊緣 : 1 (沿邊的部分) border; edge; fringe; margin; rim; limb; skirt; verge; brink; periphery 2 (靠近...
  1. 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;臺地灰泥丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與型烴源巖、深海盆地型烴源巖。
  2. 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源碎屑復理石沉積,後者為碳酸鹽巖和含碳板巖砂巖等沉積,顯示其具被動性質。
  3. The major lithofacies palaeogeographic characteristics of the qiongzhusi age and early canglangpu age ( early cambrian ) are a land in middle hubei, the carbonate tidal flat surrounding the land, shelf and a basin in the south

    早寒武世早中期巖相古地理格局由鄂中古、圍繞古的碳酸鹽潮坪、及南陸棚邊緣盆地組成。
  4. Six lithofacies palaeogeographic maps of doushantuo, dengying, qiongzhusi, canglangpu, and longwangmiao ages of late sinian and early cambrian have been made in the light of dominant facies and in the way to make stratigraphic map

    中揚子地區上震旦統發育了從碳酸鹽潮坪、開闊臺地、淺灘、臺地、斜坡到臺地前盆地等沉積,下寒武統下部主要?細碎屑巖和碳酸鹽巖組成的混合型淺海沉積,上部變成碳酸鹽潮坪、開闊臺地、臺斜坡和臺盆地沉積。
  5. In addition, by means of seismic profiles, the platform margin and the platform inner sag margin can be finally identified, integrated with distribution of organic reefs

    分析中上奧陶統烴源巖沉積環境,重要的是尋找碳酸鹽巖臺地、臺地內凹陷,從而能夠確定臺斜坡、臺地內凹陷、等烴源巖沉積環境。
分享友人