礦物時 的英文怎麼說

中文拼音 [kuàngshí]
礦物時 英文
mineral time
  • : 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...
  • : shí]Ⅰ名1 (比較長的一段時間)time; times; days:當時at that time; in those days; 古時 ancient tim...
  • 礦物 : mineral
  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組合的形成和變化的條件和過程,不同理化學條件下的成分、結構、形態、性等標型特徵以及它們之間的內在聯系,及其共生組合在間上和空間上的分佈和演化規律,成分、結構、形貌、性等的分析測試方法,地質溫度計和地質壓力計對其形成環境的表徵,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分析,重點介紹黃鐵、石英、石榴石、輝石、角閃石、雲母、長石等(族)在成因上的宏觀標志和微觀信息,以及其成因信息在成巖作用和成作用中的地質意義。
  2. The results of research on the workability of hbc concrete show that hbc concrete, when compared with opc concrete, has excellent compatibility with superplasticizer, in terms of better initial fluidity, less slump loss, definite saturation point and less dosage at saturation point. in addition, good mineral admixture such as i class fly ash can obviously improve the workability of hbc concrete. moreover, hbc concrete exhibits more excellent workability under the condition of low w / c ratio, which indicates hbc is more suitable for making super high strength concrete whose w / c ratio is very low

    對高貝利特水泥高性能混凝土工作性能的研究結果表明,高貝利特水泥與高效減水劑具有良好的適應性,表現為初始流動度較大,經損失較小,具有明顯的飽和點且飽和點摻量較小;此外,優質的摻和料如一級粉煤灰能明顯改善hbc混凝土的工作性能;更為突出的是hbc混凝土在低水膠比的情況下表現出更為優異的工作性,這一特性預示著高貝利特水泥更適宜配製水膠比很低的超高強混凝土。
  3. The rock texture , mineral occurence feature , ore electronmagnetic milling and applied possibilities in ceramics and glass of the jadeite metamorphic aegirine - augite nepheline syenite in suizhou , hubei were studied. the results show that the ore deposit combines the advantages of mining and milling , and the finished ore by single electronmagnetic milling may be fully utilized as the raw materials for ceramics and glasses. meanwhile , another important fact is that the compositon with 90 percent raw ore may be manufactured into the wall and floor tiles with glaze, which was affirmed by a lot of experiment research

    隨州硬玉質變霓霞正長巖的巖石組織結構、賦存狀態、石可選性和玻璃陶瓷原料應用試驗研究表明:該資源具有易采易選兩大優點,石經單一磁選的精可作玻璃和陶瓷的原料;同已反復試驗證實該資源可燒成原用量達90的釉面墻地磚。
  4. At the same time, the thesis has also made a discuss about the genesis of the ore belt, and brings forward a new cognition that partial aurum comes from the mantle

    ,論文還在膠東地區床成因問題上做了探討,並提出了本區金質部分來源於幔源的新認識。
  5. Features : contain lemon grass, jojoba essential oil and rich mineral deep sea salt particles, which can clean out the aged cutin on the skin surface, promote the blood circulation and metabolism, destroy and resist bug, dispel inflammation. its fresh lemon grass fragrances can dispel the beriberi and foot bad smells, clear out the bad smells, relief the tired foot, get rid out of the swollen feeling, increase the funny interests by washing foot, let the foot to recover fresh and energetic completely

    特點:蘊含的檸檬草、荷荷巴等香薰精油及含豐富質的深海鹽幼細粒子,溫和清除積聚于肌膚表面的老化角質,促進血液循環及新陳代謝,殺滅並抑制病菌,消除足部炎癥,清新自然的檸檬草芬芳,有效祛除腳氣、腳臭,清除腳部異味,同舒緩疲倦雙足,消除腫脹的感覺,增添浴足情趣,讓浸泡后的雙足徹底恢復清爽與活力!
  6. Secondly, based on the microbeam analytical technique, on the one hand, through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand, through multi - point analysis of a part of the minerals from mantle, the auther got dynamic information from mantle. finally, generalizating the fruits of this study and predecessors, the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites, clinopyroxenites, websterite, dunite, harzburgites, garnet lherzite, phlogopite lherzite, eclogites, clinopyroxene megacrysts ; compared with east china and north china platform, the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the. upper mantle beneath north hetian area is heterogeneous, with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204. 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits

    最後,綜合本區幔源和地幔巖石的特徵以及地球理資料,得出如下結論:本區上地幔的質組成有尖晶石二輝橄欖巖、二輝巖、單斜輝石巖、純橄欖巖、方輝橄欖巖、石榴石二輝橄欖巖、金雲母二輝橄欖巖、榴輝巖;與中國東部以及華北地臺上地幔相比,研究區上地幔具有富集主元素中相容元素和虧損其中的不相容元素的特徵,局部熔融程度較高;上地幔存在橫向和縱向的不均一性,從西部的克里陽到喀拉喀什河和玉龍喀什河流域, al和lree富集程度呈下降趨勢,不同來源的相同中主元素的含量差異較大;地質歷史期這里可能發生過地殼俯沖並產生殼幔混合作用;玄武巖漿的起源深度73km ;從幔源重砂的溫壓估算結果,可以推斷出巖石圈厚度可達204 . 9km ;綜合巖石圈質組成特徵、巖石圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖石和幔源的化學成分,認為研究區具備了金剛石成地幔地質條件。
  7. 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, fe ( oh ) _ 3膠體附著在巖石的表面,經過脫水結晶和吸附,形成褐鐵膠體,褐鐵膠體沿裂隙或鬆散的顆粒進入翡翠巖石中,逐漸累積沉澱,形成次生色層。
  8. The palate has a silky start and a grainy, mineral - rich finish

    入口立即感受絲般滑柔,最終有顯見大地氣味結尾。
  9. The author gives the general situation of using non - metallic minerals, such as kieselguhr, sepiolite, zeolite and bentonite, as carriers of chemical fertilizers and modifying the fertilizers to become long - acting ones, so as to cause the release of the available constituents of the fertilizers to be in balance with the crop needs, raise the use ratio of these components, and reduce environmental pollution

    筆者介紹了用矽藻土、海泡石、沸石、膨潤土等非金屬質作化肥載體,將肥料改性成為長效肥,使肥料的有效成分的釋放與作的需求平衡,以提高有效成分的利用率,同減輕環境污染的概況。
  10. The mathematical statistics method and extrema variance clustering method can be used to visible automatic classifying and reading of logging curves. the lithofacies classifying program basing on multi - mineral model analysis presents a new method to analyze logging - facies and more accuracy and visualized logging facies section can be reached by using this method. in addition, it supplies reliable lithologic layering reference for search and evaluation of oil / gas caprock and it also made up for the high cost of core - drilling and the inaccuration between lithic fragment description and depth

    採用基於「數理統計-極值方差聚類法」的面向對象可視化操作方法可有效地解決測井曲線的可視化自動分層取值問題;而基於多模型分析的巖相劃分程序又提供了一種新的測井相分析方法,能得到更為準確直觀的測井相剖面,為尋找和評價油氣蓋層提供了可靠的巖性分層依據,同彌補了鉆井取心費用高和錄井巖屑描述與深度有誤差的缺陷。
  11. If food or drinks are taken too frequently, our saliva does not have sufficient time to re - mineralize the tooth enamel, thus allowing the decay process to begin

    如果吃喝太過頻繁,唾液沒有足夠的間為牙釉質補充質,蛀牙就會發生。
  12. Fungi form mycorrhizae in plant roots and the hyphae take in carbon from plants through their epidermal cells and move mineral nutrients and water from soil to their epidermal cells ; this symbiosis is of high importance in studying biodiversity conservation, the origins and evolution of terrestrial plant, the rehabilitation and reconstruction of degenerated ecosystems, agriculture, horticulture and forestry

    真菌在植根系形成菌根后,菌絲通過根的皮層細胞獲取植提供的碳源,同營養和水從土壤轉運到皮層細胞,這種共生過程的研究在生多樣性的保護、陸生植的起源與演化、退化生態系統的修復與重建以及農業、林業和園藝業的應用具有重要的意義。
  13. 3 ) in shell of hyriopsis cumingii ( lea ), the prismatic layers and the nacreous layers are all composed of aragonite minerals, and aragonite crystallites in prismatic layers show obviously preferential orientation of [ 012 ] axis perpendicular to the shell layers, so it is considered that the orientation of aragonite crystallites in prismatic layers perhaps play an important role in deciding the orientation of aragonite crystallites in nacre and acts as one of template to resulting the formation of aragonite with [ 012 ] orientation perpendicular to nacreous layers in nacre

    3 )與海水貝殼明顯不同的是,三角帆蚌稜柱層相與珍珠層一樣皆為文石相,同查明稜柱層中文石晶體具[ 012 ]軸垂直殼層面的明顯的擇優取向。本文認為,三角帆蚌稜柱層中文石晶體的擇優取向可能對珍珠層中文石晶體的擇優取向存在模板導向的作用,導致珍珠層[ 012 ]定向的文石晶體的形成。
  14. The mineral quality with natural seaweed essence, amino acid clean elixir, the deep layer brushing dirty mark inside the pore and the surplus oleins, valid for at the same time stet the skin aqua, abundance can wake the skin vigor up, making skin feel more easily relaxed, let you own the skin color of the clearness brillancy

    成份:含天然海藻精華,氨基酸清洗劑,深層清潔毛孔內污垢及多餘油脂,同有效保留肌膚水份,豐富的質能喚醒肌膚活力,使肌膚倍感輕松舒暢,讓你擁有清爽明亮的膚色。
  15. 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

    作者還強調了成巖過程中由長石等鋁硅酸鹽溶解提供殼源sr所造成的碳酸鹽成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組成的各種分析,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。
  16. 4 ree geochemistry of fluorite, siderite, quartz, magnetite, calcite in ores mainly controlled by ore - forming fluids, in contrasting to those of the metamorphic minerals which controlled by crystal structure. the ore - forming fluids of initial stage show larger lree / hree fractionation than that of later stage. a narrow range of 6 ~ 4s valus for early stage chalcopyrite ( - 0. 3 to 2. 8 ) suggested that s originated from the mantle and the 6 13c and 8 18o valus of siderite range from - 11. 17 to - 15. 37 % and from 8 ~ 9. 1, respectively, it indicates that the c and o of ore - forming fluids were derived from the magma or organogenous sediment

    6 、昆陽群因民組地層中出現的稀土富集、成與我國的白雲鄂博稀土ree一fe一nb超大型一床和澳大利亞的olympicdamcu一u一au一ag一ree超大型一床,在成代、產出大地構造背景、成質來源等方面具有較大的相似性,均體現成受控于中元古代1
  17. According to the thermodynamics analysis of spontaneous mineral of iron, we assumed : when sewage disposal, if sulphur is eliminated prior, this makes the consistency of iron ' s ion keep high relatively, it will react with phosphorus, produce heterosite, vivianite precipitate. this will decrease the interior load of the phosphorus in sediment, and reduce the consistency of the phosphorus in the dianchi lake

    根據鐵的自生的熱力學分析,提出設想:如果在污水處理,優先脫硫,就使鐵離子的濃度保持較高,與磷生成磷鐵、藍鐵沉澱,就可以減輕沉積中磷的內源負荷,進而降低滇池湖水中的磷的濃度。
  18. It is medium - bodied with sweet, ripe black cherry and raspberry notes, some crushed rocks, and that distinctive minerality that rayas seems to provide. undoubtedly the best in rhone valley

    酒體醇厚的恰到好處,綻放出甜美圓熟的黑櫻桃與覆盆子香氣,同可感受到拉雅堡特有的新碎巖釋出的芬芳感。毫無疑問是俯瞰隆河區的唯一王者。
  19. The diageneses which are destructive to the reservoirs are mainly the filling of minerals in secondary pores, the fissures and the dissolved caverns

    對儲層起到破壞作用的主要是充填作用,表現為次生溶蝕孔隙、裂縫、溶洞中充填自生,它們的包裹體測溫數據證明充填作用發生在埋藏期。
  20. Abstract : to the principle and project that tu guangazhi proposed in 1990, the gold ore deposits in qinling ( shaanxi ) may be classified into fouowing types : archean high - grade gneiss type, fine grained fragmental rock - carbonate rock - silicilith type, metamorphic fragmental rock type, volcanic rock type, explosive breccia type, intrusive rock exo - and endo - contact zone type. inthis paper, the geological characteristics, metallogenic geological setting, the source of ore - forming materials, digenic mechanism and metallogenetic epoch of gold ore deposits are also discussed

    文摘:參照塗光熾先生( 1990 )提出的床類型劃分原則與金分類方案,將陜西秦嶺地區原生金劃分為太古界綠巖建造型、細碎屑巖-碳酸鹽巖-硅質巖建造型、變質碎屑巖型、火山巖建造型、隱爆角礫巖型和侵入巖內外接觸型金,並對各類型金的地質特徵、成地質背景、成質來源、床形成機制及形成代等問題進行了論述和討論。
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