鐵質沉積 的英文怎麼說

中文拼音 [tiězhíchén]
鐵質沉積 英文
ferriginous sediment
  • : Ⅰ名詞1 (金屬元素) iron (fe) 2 (指刀槍等) arms; weapon 3 (姓氏) a surname Ⅱ形容詞1 (形容...
  • : Ⅰ名詞1 (性質; 本質) nature; character; essence 2 (質量) quality 3 (物質) matter; substance;...
  • : 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...
  • : 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...
  • 鐵質 : human iron metabolism
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. So the effect of eutrophication of dianchi lake of sediment ca n ' t be ignored. based on the research of modern sediemnt of dianchi lake, the thesis is concerned about some physical and chemical characteristics ( including magnetic susceptibility, ammoniac nitrogen and effective phosphprus etc. ) and thermodynamics analysis of spontaneous mineral of iron

    本論文主要以滇池現代物為研究對象,對滇池現代物的主要物理和化學性(包括氨氮、有效磷、磁化率等) ,進行基礎性地分析研究並對滇池現代的自生礦物進行了熱力學分析。
  2. Sxotf is recognized in the northern qaidam based on the analysis of structures of area. this oblique trusting fault zone with northwestern - southeastern trending consists of fault gouge, fault breccia and fault cleavage. fault hanging wall consists of sertengshan - xitieshan napple, which is distribution in dextral en echelon. fault footwall consists of youcangshan formation in neogene

    本文在對賽什騰? ?錫山斜沖斷裂詳細地段構造解析的基礎上,結合盆地的特徵、地球物理資料等對該斜沖斷裂的幾何學、運動學及形成時代進行了研究,論文著重探討了賽什騰? ?錫山斜沖斷裂的地意義。
  3. 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

    周圍礦床的風化蝕變為表生水提供了,形成弱酸性的含fe ( oh ) _ 3膠體的水溶液,表生水流經翡翠礦石時, fe ( oh ) _ 3膠體附著在巖石的表面,經過脫水結晶和吸附,形成褐礦膠體,褐礦膠體沿裂隙或鬆散的礦物顆粒進入翡翠巖石中,逐漸累澱,形成次生色層。
  4. The colour of illite jade is of distinct gradation which is related to the content of hematite in different sedimentary bed

    該玉石的顏色層次結構清楚,分界明顯,與不同層中赤礦的量分數有關。
  5. The fluids upwelled to seafloor along fault thus ore - forming metals accumulated. 2. this paper indicated the definition the hydrothermal sedimentary rocks. the definition is a group of especial sedimentary rocks forming at the temperature ranging from 70 ? to 350 ? ( or more high ) through sedimentation and synsedimentary metasomatism in the seafloor

    區內的熱水巖主要有硅巖、鈉鉀長石巖、重晶石巖、透閃石巖、碳酸鹽巖、綠泥石巖和白雲石斑點千枚巖,它們往往與熱水礦體緊密伴生。
  6. A recent discovery of peridot in the cashmere region of pakistan has renewed its popularity

    的含物和白雲石灰巖中,完全由橄欖石構成。
  7. The results indicate that the jade mainly consists of illite and a small quantity of feldspar, quartz, hematite, siderite and rutile, which is argillaceous sedimentary rock

    結果表明,其礦物成分以伊利石為主,含有少量的長石、石英、赤礦、菱礦和金紅石,為泥巖。
  8. Abstract : based on 1 200000 aeromagnetic survey data performed in 1998, and referred to materials of geolo - gic and geochemical prospecting of the working area, this paper discusses the relationship between the characte - ristics of magnetic field, magmatic rocks, fault structure and the distribution of mineral resources, and investigates the geologic metallogenic environments, and sets up the prospecting criteria for hydrothermal and volcanic - sedimentary copper, lead, zinc, gold, iron, manganese deposits, then makes the prognosis of the prospecting potential of the working area

    文摘:本文以1998年1 20萬航空磁測資料為基礎,參考地和化探資料,對工作區磁場特徵、巖漿巖、斷裂構造與礦產分佈的關系進行探討,研究地成礦環境,建立尋找熱液型和火山-型的銅、鉛、鋅、金、、錳礦找礦標志,對本區找礦遠景進行了預測。
  9. Dlc can be deposited on various substrate with excellent adhesion such as steel, titanium alloy, aluminum alloy and cemented carbide, etc

    可以在各種鋼、鈦合金、鋁合金、硬合金等多種材料上,結合力好。
  10. In this paper, the authors used such geophysical exploration methods as the high - precision geomagnetic method, the resistivity profiling method and the induced polarization method to synthetically study the exhausted areas of the archean sedimentary metamorphic iron mines in eastern hebei, built an effective geophysical exploration combination model for the exhausted areas, and summarized the serviceability and validity of various geophysical exploration methods in the exploration of exhausted areas under different geological settings

    摘要應用高精度磁法、電阻率剖面法、激發化法等常規地球物理勘查方法對冀東地區太古宙礦采空區進行綜合研究,建立冀東礦采空區有效的地球物理勘查組合模型,總結不同地環境條件下各種地球物理勘查方法在冀東礦采空區勘探中的適用性和有效性。
  11. In recent years, during construction of railway in the southwest mountain area, we encountered the soft and weak soil that distributes on the slope and is similar with physical mechanical index of soft soil of marine deposit, lake deposit, etc., but different in cause of formation, scope of distribution, composition of mass and others characteristics. to emphasize its characteristics of distribution, we call it as " soft soil on the slope "

    近幾年,在我國西南山區路建設中,常遇到一種分佈在斜坡上的軟弱土,它與海相、湖相等的軟土物理力學指標相似,但在形成原因、分佈范圍、物組成及其它特性上又有所區別,為強調其分佈特徵,我們稱其為「斜坡軟土」 。
  12. The results indicate that submarine hot water deposition is the main ore - forming process of the uranium - bearing vonsenite deposit, and that the economic deposit was formed on the basis of further enrichment of boron and iron through the superposition and transformation by regional metamorphism and migmatization

    研究表明,該礦床的成礦作用主要表現為海底熱水成礦,區域變混合巖化作用對礦床進行了強烈的疊加改造,使硼進一步富集而形成工業礦床。
  13. By study dabaoshan deposit on minerogenetic and geological background, mineral constituent, rare - earth element, isotope and typomorphic feature of sulpurization mineral, finally, we made a conclusion that dabaoshan deposit resulted from the volcanic deposition which type is laterebuilt and magma hydrothermal superimposed. we found the upside of dabaoshan deposit have been denuded or oxidized, bassically, it have reached the lowest part of the deposit

    通過對大寶山礦床的成礦地背景、礦物成分、稀土元素組成、同位素以及黃礦、閃鋅礦、方鉛礦的標型特徵進行研究,確定了大寶山礦床的成因為火山,經後期巖漿熱液疊加型礦床,對礦床的遠景進行了預測,提出大寶山礦床的上部礦體已被剝蝕或被氧化,基本上已經到礦體的深部的觀點。
  14. In 2005, 61 physical and chemical parameters were measured and analysed in sediments. these included particle size, electrochemical potential as highly anoxic sediment with negative potential is related to organic pollution, chemical oxygen demand which indicates organic pollutants, total sulphide inorganic constituents, source of the unpleasant - smelling gas hydrogen sulphide, 15 metals and metalloids aluminium, arsenic, barium, boron, cadmium, chromium, copper, iron, lead, manganese, mercury, nickel, silver, vanadium and zinc, and trace toxic organics pahs and pcbs - 16 compounds and 18 congeners respectively

    2005年,物監測包括分析61種物理及化學參數,其中有粒子大小電化學勢有機污染促使物缺氧,而讓電化學勢呈負數值化學需氧量顯示有機污染程度總硫化物無機物,是造成難聞氣體硫化氫的主因15種金屬及準金屬鋁砷鋇硼鎘鉻銅鉛錳汞鎳銀釩及鋅和痕量毒性有機物多環芳烴及多氯聯苯分別為16種復合物及18種同物。
  15. This paper analyzes and studies the project quality of china railway no. 14 group no. 2 company. on the base of research, the paper also, points out no. 2 company ' s unsolved problems for a long time such as the reason of project quality accident and accident tendency

    本文在充分調研的基礎上,對中十四局集團二公司施工項目的量管理進行了分析、研究,指出了二公司長期未解決的較突出的問題,工程量事故和事故苗頭還沒有從根本上得到遏制的原因。
  16. ( 5 ) according to the study on seismicic data, sedimentary characteristics, contact relations, incision relation of the faults and strata related to the folds which are associated with the faults, this paper reached the conclusions : the oblique - thrusting structure of sertengshan - xitieshan in northern qaidam basin was formed in middle jurassic and the left - thrusting fault zone was established in the late pliocene of neogene

    ( 5 )根據地震料、特徵、地層的接觸關系、斷裂切割地層關系以及與斷裂相關的褶皺捲入地層的研究,認為柴達木盆地北緣的賽什騰? ?錫山逆沖推覆構造形成於中侏羅世,而左行逆沖斷裂帶定型于新第三紀上新世末。
  17. The ratio of y / ho in ores approximates to the ratio of black chimney in tag seafloor. the ore - forming fluids show high temperature and redox characteristics. in conjunction with the geological setting of the deposit, the primary ore - forming fluids might certain higher ree and higher volatile elements derived from the mantle degassing or the alkaline volcanic magmas

    同時結合礦床形成的構造一地環境及礦體產出的地形態,認為迅納廠稀七銅礦床可能是在昆陽裂谷初期,在堿性火山巖漿噴發的間歇期,來自地慢富稀土、揮發份的成礦流體山火山噴流一同生方式形成的礦床。
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