磷塊巖 的英文怎麼說
中文拼音 [līnkuāiyán]
磷塊巖
英文
phosphatic rock-
Characteristics and phosphogenesis of phosphorite of the sinian - cambrian, west yangtze area
寒武紀磷塊巖巖石學特徵及成因分析Uranium is frequently enriched by sorption or chemical combination in shales, lignites and phosphorites.
鈾經常為頁巖，泥炭和磷塊巖所吸附或化學結合態而富集。Phosphorite ; upwelling ; hot spot activity
磷塊巖上升洋流熱點活動The phosphorite and genesis of industrial p deposit in east yunnan
滇東磷塊巖及工業磷礦床成因Ree geochemistry of doushantuo phosphorites and paleoenvironmental changes in weng ' an area, south china
貴州甕安陡山沱組磷塊巖的稀土元素地球化學特徵與沉積古環境Rees geochemistry of doushantuo phosphorites and modification during post sedimentary stages in weng ' an area, south china
貴州甕安陡山沱組磷塊巖稀土元素地球化學特徵與沉積期后變化On the basis of studying on baiguoping phosphate deposits cadmium geochemical characteristics, the significance of studying on cadmium supergene geochemistry activation course in phosphate rock deposits is discussed
摘要通過對白果坪磷礦床中鎘地球化學特徵的研究，探討了對磷塊巖礦床中鎘的表生地球化學作用過程研究的意義。Double - reverse flotation process of phosphate rock that contains silica and calcia
某硅鈣質磷塊巖雙反浮選工藝研究Test of leaching rare - earth elements from phosphate rock containing rare - earth elements
含稀土磷塊巖稀土浸出探索性試驗Cadmium is existed in phosphate rock as isomorphism and sorption state, while cadmium is existed in weathered phosphate rock chiefly as sorption state
鎘在磷塊巖中的賦存狀態為類質同象和吸附態，在風化磷礦石中以吸附態為主。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，被剝蝕下來的產物成為潮坪型磷塊巖的主要磷質來源，在碳酸鹽巖臺地發生的熱點活動和上升洋流從盆底深部帶來的磷質，共同作為臺地型磷塊巖的磷源，盆地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積環境中，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。分享友人