蝕積臺地 的英文怎麼說

中文拼音 [shítáide]
蝕積臺地 英文
cut and built platform
  • : Ⅰ動詞1. (損失; 虧耗) lose 2. (腐蝕) erode; corrode Ⅱ名詞(天體現象) eclipse
  • : 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...
  • : 臺名詞(指臺州) short for taizhou (in zhejiang province)
  1. The field observation of the sediments of storm surge produced by no. 11 typhoon in 1997 shows that sedimentation rate of storm surge sediments are greater than that of normal astronomical tide sediments, and the grain size shows relative coarse with poor sorting. vertical sequences of the storm sediment show parallel bedding and overlapped by hummock bedding. these characteristics provide good basis for building the index of storm surge deposit

    通過對梁垛河閘9711號風的現場觀測並結合目前已有的風暴潮沉的研究,分析了風暴潮沉在構造和結構上的特點,從而建立了正常潮灘沉中風暴潮沉的識別標志,同時在野外觀測中還發現即使在風暴潮期間,高潮灘上部仍存在只有淤沒有侵帶。
  2. The favorable reservoir spaces in the carbonate rock could be divided into five types according to their origin, configuration and size, i. e., solution fissure, solution hole, cave, erosional fissure and structural fissure, which form five different reservoirs including cave - type reservoir, erosional fracture reservoir, structural fissure reservoir, and solution pore marginal beach grainstone reservoir

    而下奧陶統灰巖段儲集和生產油氣的有效儲滲空間按成因、形態及大小可劃分為溶孔隙、溶孔洞、大型洞穴、風化裂隙、構造裂隙等5類,構成5種性質有別的儲層,即洞穴型儲層、風化裂隙型儲層、構造裂隙型儲層、緣灘相顆粒灰巖溶孔隙型儲層和表殘物裂隙孔隙(洞)型儲層。
  3. Cut and built platform

    蝕積臺地
  4. Phosphate deposits are distributed along the margin, platform and basin in the west yangtze area. the analysis methods include the paleogeography, petrology, organic geochemistry, geochemistry. the conclusions are drawn that the source of phosphate deposits distributed along the margin originate from the weathering production of continent, while phosphate deposits along the platform and basin gain phosphorus through hot spring on the buttom of the sea floor, which is brought to the sedimentary environment by rising sea - fluid, then accumulated by the organism and microorganism, meanwhile, basin phosphorite keep relatively higher organic carbon content

    認為早寒武世早期古陸遭受風化,被剝下來的產物成為潮坪型磷塊巖的主要磷質來源,在碳酸鹽巖發生的熱點活動和上升洋流從盆底深部帶來的磷質,共同作為型磷塊巖的磷源,盆型磷塊巖的磷質同樣是由熱點活動和上升流攜帶至缺氧的沉環境中,通過藻類或微生物的富集作用成巖,並保留了較高的有機碳含量。
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