礦石沉澱 的英文怎麼說

中文拼音 [kuàngdànchéndiàn]
礦石沉澱 英文
ore emplacement
  • : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
  • : 石量詞(容量單位, 十斗為一石) dan, a unit of dry measure for grain (= l00 sheng)
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • 礦石 : ore; mineral
  • 沉澱 : 1 (沉澱過程中析出的物質) sediment; precipitate; sedimentary accretion; precipitation; (doposit...
  1. Silica pigment, benzene parazolone, oxalic acid catalyzer, accelerant, catalyst, deposit carbon powder, starch, paraacetaminophenetol - sulfonamide, sodiumpara - aminosalicylate ( pasna ), dalmato, p - thephalic acid, diethylbenzene - amine, titanium dioxide, acticarbon, sodium fluosilicate, fluorite, by - thiamine, silica gel powder, synthetic resin, sulfonic acid, polypropylene resin, aureomycin, pyrosodium silicate, gluchlorine acid coffee grounds, glucose, sodium sulfate, sulfide mineral, guound phosphate rock, bb, p. v. c.,

    M 、觸媒、炭粉、對乙酰氮基苯磺酰氨、對氨基水楊酸、哆耳瑪托、對苯二酸、二乙苯銨、二氧化鈦、活性碳、氟硅酸鈉、氟、副產硫銨、硅膠粉未、合成樹脂、磷酸鈣、聚丙烯樹脂、金黴素、偏硅酸鈉、糠氯酸咖啡渣、口服葡萄糠、硫酸鈉、硫化、磷粉、蘭bb 、 p . v
  2. By infrared spectrum study, the limonite ( feooh nh2o ) can be considered the main colorating mineral in the yellow and red jadeite, and the hematite is another colorating mineral in the red jadeite. the difference of color tone is due to the n value in the molecular formula feooh nh2o and the content of crystal water and adsorbent water. the iron ion came from the effloresced and eroded rocks, and formed fe ( oh ) 3 colloid reacted with the surface water

    周圍床的風化蝕變為表生水提供了鐵質,形成弱酸性的含fe ( oh ) _ 3膠體的水溶液,表生水流經翡翠時, fe ( oh ) _ 3膠體附著在巖的表面,經過脫水結晶和吸附,形成褐鐵膠體,褐鐵膠體沿裂隙或鬆散的物顆粒進入翡翠巖中,逐漸累積,形成次生色層。
  3. According to the analysis on the lithogeochemical features and the carbon and oxygen isotopes of calcareous sandstones, it is realized that there some genetic relation between the formation of calcareous sandstone and uranium mineralization in the oxidation - deoxidation transitional belt, that is the precipitation and enrichment of uranium is accompanied by the deposition of carbonate and formation of calcareous sandstone

    根據鈣質砂巖的巖地球化學特徵,結合碳、氧同位素分析認為,氧化還原過渡帶中鈣質砂巖的發育與鈾化的形成具有一定的成因聯系,即在鈾富集成的同時,伴隨著碳酸鹽的析出作用,形成鈣質砂巖。
  4. Porcelain stone exploited from a mine is changea into brick - form mud block, through the processes of water - ramming, washing, decontaminating, and depositing. then, the mud bolck is treated with water for farther decontaminating, and is twisted with hand or treaded with feet for squeezing air out of the blocks and for distributing water content well in the block

    區採取瓷,經水碓春細,淘洗,除去雜質,后製成磚狀的泥塊。然後再用水調和泥塊,去掉渣質,用雙手搓揉,或用腳踩踏,把泥團中的空氣擠壓出來,並使泥中的水分均勻。
  5. With the intermittent activity of hot fluid containing cc ^, ferrous carbonate minerals dissolved and precipitate repeatedly many times. in addition, dissolution of shells and feldspars, decrease of chlorite and increase of kaolinite could be found

    隨著富co _ 2熱流體多次間歇性入侵導致了含鐵碳酸鹽物的反復多次溶解和、生物介殼大量溶蝕和長鑄模孔的形成以及綠泥消失、高嶺增加等。
  6. Main content in simulation is the spatio - temporal evolution of the set of descriptive variables characterizing tectonic mineralization state under coupling of various processes as following : ( 1 ) variables related to forming and property of ore - forming fluid, such as dissolution rate of minerals ( include metal minerals ) in rock, concentration and saturation of aqueous species in fluid, temperature, pressure, and ionic strength etc. ; ( 2 ) variables related to structural deformation and fluid flow, such as stress, deformation rate, fracture network, porosity, fracture permeability ; ( 3 ) variables related to precipitation and mineralization, such as nucleation rate of gangue and metal minerals, accumulation precipitation of various minerals, etc. ; ( 4 ) spatio - temporal coupling relation of various variables above, such as the coupling relationship between spatio - temporal evolution of fracture permeability and flow and focus of fluid and ore - forming

    模擬的主要內容是在各種過程耦合作用下,以下描述構造成體系的主要變量的時空演化:與成流體的形成和性質有關的變量,如地層中物(包括成物質)的溶解速率、流體中各組分的濃度與飽和度、流體溫度、壓力、離子強度等;與構造變形和流體運移有關的各變量,如應力與變形速率、巖孔隙度、構造(斷裂)滲透率等;與有關的變量,如物(金屬物和脈物)的成核速率、各物的量等;上述各有關變量間的時空耦合關系,如斷裂滲透率時空演化與流體流動、匯聚和成的耦合關系等。
  7. This process was propitious to enrich, activate, transport the copper. in different alteration granodiorite porphyry, sio2, k2o, cu, mo are depleted in the fresh and weakly altered rock, and are enriched in the strongly altered rock, cl is also enriched in the strongly altered rock. but na2o and fe are extracted from the porphyry into the ore - forming fluid, especially the presence of fe is in favor of cu deposition

    在銅廠巖體不同的蝕變帶中, sio _ 2 、 k _ 2o 、 cu 、 mo等從新鮮斑巖甚至弱蝕變帶中帶出,而在強蝕變帶強烈富集, cl同樣有在強蝕變巖中富集的趨勢;而na _ 2o 、 fe從斑巖體中帶出,進入流體相中,流體中大量fe的存在,有利於銅的、富集成
  8. Standard practice for preparation of natural - matrix sediment reference samples for major and trace inorganic constituents analysis by partial extraction procedures

    使用部分萃取法的大量和微量無機成分分析用天然雜礦石沉澱物標樣制備的標準實施規范
  9. Chemical analysis of zinc ores concentrates. accurate determination of zinc by complexometric titrimetry after complete precipitation of interfering elements

    的化學分析.雜質完全後用絡合滴定法進行鋅的精確測定
  10. On the contrary, the reservoirs that were not influenced by hot fluid just were in early diagenetic stage b. 2. based on the synthetic analysis of varied data, the mechanism of repeated dissolution and precipitation of ferrous carbonate minerals has been discussed

    在進行充分的巖學研究基礎上,利用電子探針、穩定同位素及包裹體分析數據,探討了異常成巖演化儲層中含鐵碳酸鹽物反復溶解和的機理。
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