礦物組成分析 的英文怎麼說

中文拼音 [kuàngchéngfēn]
礦物組成分析 英文
mineralogical analysis
  • : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
  • : 名詞1 (東西) thing; matter; object 2 (指自己以外的人或與己相對的環境) other people; the outsi...
  • : Ⅰ名詞1 (由不多的人員組成的單位) group 2 (姓氏) a surname Ⅱ動詞(組織) organize; form Ⅲ量詞(...
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : 分Ⅰ名詞1. (成分) component 2. (職責和權利的限度) what is within one's duty or rights Ⅱ同 「份」Ⅲ動詞[書面語] (料想) judge
  • : Ⅰ動詞1. (分開; 散開) divide; separate 2. (分析) analyse; dissect; resolve Ⅱ名詞(姓氏) a surname
  • 礦物 : mineral
  • 組成 : form; make up; compose; formation; composition; configuration; make-up; compo
  1. In the course, the condition and the process of forming and changing of minerals, the typomorphic features of minerals, the characteristics of the distribution and the evolution of minerals and their paragenetic associations in the period and the space, the methods of mineral analyses and research, the geological thermometers and the geologicial barometers of minerals, mineral paragenetic associations and paragenesis analyses will be introduced, and the magnificent and the microscopic genetic characteristics of pyrite, quartz, garnet, pyroxene, amphibole, mica, feldspar, and other minerals will be dealt with particularly

    本課程主要講述及其共生合的形和變化的條件和過程,不同理化學條件下、結構、形態、性等標型特徵以及它們之間的內在聯系,及其共生合在時間上和空間上的佈和演化規律,、結構、形貌、性等的測試方法,地質溫度計和地質壓力計對其形環境的表徵,不同體系(封閉體系、開放體系)條件下,的穩定范圍和彼此替代順序的共生,重點介紹黃鐵、石英、石榴石、輝石、角閃石、雲母、長石等(族)在因上的宏觀標志和微觀信息,以及其因信息在巖作用和作用中的地質意義。
  2. It focuses on the theory of the mineral functional materials " improving the anti - chloride permeability and the chloride binding. the main achievements of this article include : 1 ) use the technology of xrd, sem, bet, laser particle size distributor etc to test the component, the construction, particle size distributor, specific surface etc of micro - silica, ultra - fined slag, high quality fly ash, meta - kaolin clay, four types of the mineral functional material, theoretically analysis the functions which the four mineral functional minerals act on cement concrete, namely pozzolanicity effect, filling effect, micro - aggregate effect, surface adsorption effect and so bring into play the affect of plastification, lowing of temperature, reinforcement, improvement of durability. base on this analysis we can conclude that the proper diameter of the mineral functional material is 5 m - 15 m, that is blain fineness 4500cm2 / g - 7500cm2 / g

    本論文的主要果包括以下幾個方面: ( 1 )採用xrd 、 sem 、 bet 、激光粒度儀等多種測試手段,探明了以硅灰,超細磨粒化高爐渣,優質粉煤灰及偏高嶺土超細粉等4種超細功能材料的、結構、粒度佈、比表面積等基本性質;從理論上功能材料在混凝土中的4種效應,即火山灰效應、填充密實效應、微集料效應、表面吸附效應,並由此發揮出增塑、溫峰削減(降熱) ,增強及耐久性改善等作用;通過相關理論,推導出功能材料的合理粒徑范圍在5 m 15 m ,即勃氏比表面積為4500cm ~ 2 g 7500cm ~ 2 g 。
  3. This paper emphasizes the effect of the dissolution of aluminosilicate during diagenesis may provide more radiogenic strontium which would result in a high content of strontium in carbonate rocks. so we should avoid the vein of carbonate and select the samples with less terrigenous clastic, less grain content and lacking calcite cementation collected as analysis samples. the microcrystalline limestone and micro - to fine - crystalline dolomite are rather fairly whole rock samples

    作者還強調了巖過程中由長石等鋁硅酸鹽溶解提供殼源sr所造的碳酸鹽巖蝕變可能表現為較高的sr含量;因此,在用全巖樣品進行旨在反映海水的各種時,應迴避碳酸鹽脈,選擇含陸源碎屑低、顆粒數量少、缺乏方解石膠結的樣品,微晶灰巖或微?粉晶白雲巖是較為理想的全巖樣品。
  4. The authors studied the characteristics of element geochemistry, mineral assemblage and microtexture of the white reticulate clay in the quaternary laterite of the dongting basin with some experimental analysis methods, such as chemical analysis, x - ray diffraction analysis, ir and sem analysis. the genesis of the vermiculate reticulate clay and the rhizomatic reticulate clay in the quaternary laterite of the dongting basin are discussed. the formation of crannies or holes in the soil and the transference of soil elements are absolutely necessary conditions to form the white reticulate clay in laterite

    在野外考察的基礎上,運用化學全量x射線衍射紅外光譜和掃描電鏡微形貌等實驗方法和手段,對洞庭盆地第四系紅土地層中網紋的元素地球化學合特徵和微形貌特徵進行了系統研究,對洞庭盆地紅土地層中2種主要的網紋類型蠕蟲狀網紋和根狀網紋的因進行了探討。
  5. The paper introduced in brief the basic chemical and mineral component, and analysed the effect and the evaluation index of the chemical component, vitreous body quantity and structure and the fineness degree of the phosphorus slag on its chemical activity, and finally, discussed the effect of phosphorus slag as additive on cement hydration property and the micro structure of the harding body

    摘要簡要介紹了磷渣的基本,包括化學了磷渣的化學、玻璃體數量和結構、磷渣細度對其化學活性影響及其評價指標;探討了磷渣用作水泥混合材對漿體水化性能和硬化體微觀結構的影響等。
  6. Based on the study of geologic characteristics, such as mineralogic assembladge, structural and textural features of granite of guidong granitic massif, and by using petrochemical, trace - element and isotopic data, and some petrochemical, trace - element and isotopic diagrams widely applied to the identification of geo tectonic environments, authors recognize that guidong granitic massif was emplaced in post - orogenic collision environment

    摘要本文在研究貴東花崗巖巖體巖石合、結構構造等地質特徵的基礎上,運用花崗巖的巖石化學、微量元素和同位素等數據,採用目前廣泛應用的幾種巖石化學圖解、微量元素和同位素圖解等方法,判別了貴東巖體形的構造環境?造山帶后碰撞型。
  7. Potash micatization is one of the main hydrothermal alteration minerals genetically related to the lead - zinc - silver deposit. it usually shows as muscovitization, sericitization and illitization. this paper presents a comprehensive study on the chemical composition of potash mica, adapted the follow methods : electronic probe, differential thermal analysis, x - ray diffraction analysis. at last, the structu ral characteristics and the geological environment of potash mica forming have been discussed

    系統地研究了鉀質白雲母化的,採用了電子探針差熱x射線等技術方法,探討了鉀質白雲母的結構特徵和形的地質環境及找意義。
  8. The main principle problems in the study area include, the diagenetic history, the type of sandstone, the source of the sandstone type, the source of cement, the source rocks for generation petroleum, the formation of secondary porosity, the oil migration, and reservoir quality

    論文在油體系的基本思路指導下,探討東營凹陷南部斜坡帶孔店儲集砂巖的源方向、膠結作用、巖作用動力學過程,以及次生孔隙發育與油氣生聚集的關系。
  9. Abstract : the petrologic characteristic and the pore types of y8 y10 reservoir are studied by x - ray diffraction method, the quantitative mineral clay analysis method and thin - section analysis method. based on the study, the mistakes are corrected in the naming of the sandstone and in the composition of the pore filling substance. the pore characteristic of the sandstone and the main factors of controlling the pore development are discussed

    文摘:利用x衍射全巖方法、粘土定量方法和薄片鑒定等方法研究了城華地區延8 -延10儲層巖石學特徵和孔隙因類型.綜合論述了城華地區延8延10油不同巖相儲層砂巖的基本特徵,糾正了砂巖定名的錯誤和主要填隙份的錯誤,同時還論述了儲層砂巖的孔隙特徵和控制孔隙發育的主要因素
  10. The petrologic characteristic and the pore types of y8 y10 reservoir are studied by x - ray diffraction method, the quantitative mineral clay analysis method and thin - section analysis method. based on the study, the mistakes are corrected in the naming of the sandstone and in the composition of the pore filling substance. the pore characteristic of the sandstone and the main factors of controlling the pore development are discussed

    利用x衍射全巖方法、粘土定量方法和薄片鑒定等方法研究了城華地區延8 -延10儲層巖石學特徵和孔隙因類型.綜合論述了城華地區延8延10油不同巖相儲層砂巖的基本特徵,糾正了砂巖定名的錯誤和主要填隙份的錯誤,同時還論述了儲層砂巖的孔隙特徵和控制孔隙發育的主要因素
  11. According to the comparison and analysis of mineral composition and geochemical characteristics of trace element, sulfur isotope, hydrogen and oxygen isotope, lead isotope and rare earth element in the gold ore and the altered spilite from the deposits of huachanggou gold mine, it was confirmed that the gold ore had obvious succession of the basic igneous rock

    摘要通過對鏵廠溝金床金石和蝕變細碧巖、微量元素、硫同位素、氫氧同位素、鉛同位素及稀土元素地球化學特徵地對比,得出金石對該基性火山巖存在明顯的繼承性。
  12. The lab tests contained soil dynamic triaxial test, x ray diffraction, scanning electronic microscope observation, grain size analysis and routine soil tests

    室內測試主要有土樣動三軸實驗,x衍射,土樣微結構掃描電鏡觀測,土樣粒度和常規土工實驗
  13. Mineral compositions and the microstructure were investigated by xrd and sem ; the result show that the second phase and liquid phase are produced during sintering, and the second phase and liquid phase were filled in space of the al2o3 crystals, which can control the microstructure efficaciously

    通過xrd 、 sem (帶能譜)等測試手段測試樣品的和顯微結構;結果表明,引入mgo等化劑后,材料在燒結過程中主要形第二相和一定量的低共溶相填充在al _ 2o _ 3晶粒之間,籍此可以有效控制材料的顯微結構。
  14. Prospecting indicator of jadeite in burma and perspective zones in china

    翡翠及相關玉石飾品的及含量激光拉曼光譜無損
  15. Analysis on compositions of clay minerals in black soil of central jilin, china

    吉林省中部黑土黏粒
  16. Powder x - ray diffraction analysis and micro - raman spectra were used to study the mineral composition of chinese freshwater cultured pearls from zhuji, zhejiang province

    摘要採用粉末x射線衍射及顯微激光拉曼光譜對三角帆蚌養殖珍珠的進行了研究。
  17. This paper is based on a great deal of on - the - spot data in some basins. log cores from twenty wells are selected to perform clay mineral composition analysis, shape and structure of slice core analysis, and sensitivity analysis

    本文根據某盆地大量現場施工資料,選取20口井的巖心,進行了其粘土礦物組成分析、巖心薄片形貌及結構,以及敏感性特徵
  18. The occurrence, mineral composition and constructure of titanium in solidified slags which are obtained from blast furnace slags via selective precipitating and growth have been studied, and the contribution of titanium among different mineral phases has been calculated by optical microscope, x - ray diffraction ( crd ) as well as scanning electron microscope ( sem )

    本文採用光學顯微鏡、 x射線粉晶衍射、圖象和掃描電鏡等多種手段,研究了攀鋼含鈦高爐渣經選擇性出處理的凝渣中鈦的賦存狀態、及結構,計算了鈦在各相中的佈,測定了原料中鈦的解離度,為鈦的綜合利用提供了科學依據。
  19. Abstract : the occurrence, mineral composition and constructure of titanium in solidified slags which are obtained from blast furnace slags via selective precipitating and growth have been studied, and the contribution of titanium among different mineral phases has been calculated by optical microscope, x - ray diffraction ( crd ) as well as scanning electron microscope ( sem )

    文摘:本文採用光學顯微鏡、 x射線粉晶衍射、圖象和掃描電鏡等多種手段,研究了攀鋼含鈦高爐渣經選擇性出處理的凝渣中鈦的賦存狀態、及結構,計算了鈦在各相中的佈,測定了原料中鈦的解離度,為鈦的綜合利用提供了科學依據。
  20. Among them the x - ray diffraction analysis is mainly used to confirm clay mineral assemblages and their crystallinity ; chemical analysis and electronic microscope are used to study the source, the genesis and the evolvement process of clay minerals ; radioactive isotopes analysis can make up the relationship between the time and space which is based on the climate index and the chronology ; hydrogen and oxygen isotopes also provide important evidence for reconstructing paleoclimate

    其中, x射線衍射主要用來確定黏土合及其含量以及某些黏土的結晶度化學電鏡主要用於黏土的來源因演變過程的研究放射性同位素的研究使氣候指標和年代學建立起時間和空間上的聯系而氫氧同位素亦能對古氣候重建提供重要佐證。
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