礦脈石英 的英文怎麼說
中文拼音 [kuàngmàidànyīng]
礦脈石英
英文
vein quartz- 礦 : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
- 脈 : 脈名詞1. (動脈和靜脈的統稱) arteries and veins2. (脈搏的簡稱) pulse 3. (像血管的組織; 連貫成系統的東西) vein
- 石 : 石量詞(容量單位, 十斗為一石) dan, a unit of dry measure for grain (= l00 sheng)
- 英 : 名詞1 [書面語] (花) flower 2 (才能或智慧過人的人) hero; outstanding person 3 (英國) britain...
- 礦脈 : [采礦工程] mineral vein; mineral ore; reef; ore vein; ore lode; vein; lode; wythern; roke
- 石英 : quartz; silici-; 石英電子手錶 crystal-oscillator watch; [鐘] quartzcrystal watch
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The metallic mineral has very few content ( 1 % - 2 % ), the mineral of ore is mainly of pyrite, chalcopyrite, limonite, aurum and electrum etc. the gangue mineral is composed of chalcedony, micro grained quartz, calsite, sericite, adularia, aragonite, chlorite, laumontite, pyrophyuite, kaolinite and so on, which show the typical mineral assemblage of epithermal
礦石為典型少硫化物型,金屬礦物含量極少( 1 - 2 ) ,主要有黃鐵礦、黃銅礦、褐鐵礦和自然金、銀金礦等。主要脈石礦物有玉髓、微粒石英以及方解石、絹雲母、冰長石、文石、綠泥石、濁沸石、葉臘石、高嶺石等,屬典型低溫礦物組合。Gold ore main type is auriferous quartz vein type
金礦床主要為含金硫化物石英脈型。Characteristics and enrichment regularities of auriferous quartz veins at the tiepo gold deposits, tianzhu, guizhou
貴州天柱鐵坡金礦含金石英脈的特徵及富集規律Analyse of fractal and chaotic characteristics for the thickness - distributions of auriferous - quartz - veins in xiangxi au deposit, hunan, china
湘西金礦含礦石英脈厚度變化的分形和混沌分析It is further indicated by the fusion of various geo - factors that the major targets include gold - bearing limonitic cataclastic rock in ningwei domain, auriferous quartz in nanhua mountain and xihua mountain domain, where the 50 - 85 strike mylonite and sulfur - bearing quartz - calcite veins of cataclastic rock is the prior ore - search targets
同時,通過多源地學因素的融合還顯示,寧衛地區找金的主攻對象以含金褐鐵礦化碎裂巖為主,南華山、西華山地區以脈型金礦為主,且重點應在50 - 85度方向糜棱巖、碎裂巖帶中尋找含硫化物的石英-方解石脈。It is proved that the electric conductivity of ore - forming solution can be used to seek for ore - forming fractures, to select the best mineralization section, to distinguish industrial and non - industrial auriferous quartz veins, to reflect the rich or poor levels of orebodies, to evaluate the stability of orebodies, to judge the denuding levels of ore veins, and to prospect the mineralization in depth
實踐證明,該方法在以下幾個方面具有應用前景: ( 1 )查找成礦斷裂,優選最佳成礦區段; ( 2 )區分有無工業價值的含金石英脈; ( 3 )反映礦段或礦體的貧富程度; ( 4 )評定礦體的穩定性或礦化不均勻性; ( 5 )評估礦脈的剝蝕程度; ( 6 )礦脈深部成礦預測。Study of short - chain carboxylates in ore - forming fluids of gold - bearing quartz veins in the southeastern guizhou
黔東南某些含金石英脈成礦流體中的短鏈羧酸Short - chain carboxylates ; fluid - inclusions in minerals ; ion - chromatography ; leachates ; gold - bearing veins
短鏈羧酸礦物流體包裹體離子色譜浸取液含金石英脈Minerals in deposit are made up simpler, the metal minerals are pyrite, chalcopyrite in second, and littler natural gold ; the veinstone minerals are quant, feldspar and carbonate
礦床礦石礦物組成較簡單,金屬礦物以黃鐵礦為主,其次為黃銅礦,有一定量的自然金;脈石礦物以石英、長石、鐵碳酸鹽為主。Chener gold deposit is located in north of xunmadao fault, the types of ore are gold - brazil - quartz of vein and gold - multimetal - quartz of vein. the occurrence of gold - bearing quartz vein is controlled by ductile - brittle shear zone, most the occurrence of gold - bearing quartz vein included by schistous zone and cracked zone, in the strike direction of gold - bearing quartz vein, it " s high content and great thickness appear on nww, in the direction of tilt, it " s high content and great thickness appear on the part of transformation from big angel of tilt to small angel of tilt
礦石類型為金-黃鐵礦-脈石英型和金-多金屬硫化物-脈石英型。含金石英脈受韌-脆性剪切帶控制,主要賦存於片理化帶與破碎帶中。在脈體走向上,北西西向脈體品位高,礦體厚度大;在傾向上,南傾,傾角較緩處品位高、礦體厚度大。According to granite ages cutting ruptures, mineralized quartz veins ages corresponding to fold deformation and formation ages of bilateral faulted basin, deformation age are limited, that are 100 ~ 65ma for one and form 65ma to the present for two and three
根據斷裂截切的花崗巖體年齡、同期褶皺變形的含礦石英脈年齡以及斷裂兩側斷陷盆地的形成時代,大致限定第1期變形時代為100 65ma ,第2 、 3期變形時代為65ma現今。In the process of writing paper, assimilating sufficiently procedessor " research achievement, exertting ductile - brittle shear zone, resolving mechanism of formation of gold - bearing quartz vein of chener. lining out ductile - brittle shear zone of chener gold deposit, presenttig pattern of controlling chener gold deposit, with analyzing of dominant ore vein - q507, graph of change of trace element on different spot level and graph of change of gold element of different construct, researching construct geochemistry of ore zone
在論文撰寫的過程中,充分吸收前人的研究成果,運用韌性剪切帶理論,解析了陳耳金礦區含金石英脈體的形成機理,劃出了控制陳耳金礦床的韌-脆性剪切帶,提出了礦床的構造控礦模式。From the study of lanthanon, we know that quart - vein is the single production of hydro mineralization. etch rock and mineralized rock are the mix outcome of hydro mineralization and wall rock materials
稀土元素研究結果反映石英脈是成礦流體的單純產物,而蝕變巖和礦化巖石則是成礦流體與圍巖物質的混合產物。The useful ore mineral is barite and the gangue minerals are mainly calcite, clay mineral and quartz et al
礦石礦物為重晶石,脈石礦物主要有方解石、粘土礦物和石英等。The genesis of gold deposits is complex in this district, the type of quart - vein plus etch rock belongs to hydro thermally superimposed complex mineralization. the type of porphyry and scraping rock containing charcoal belongs to volcano sediment - alteration hydro thermally gold deposits, the formation of gold deposits is controlled by several factors
本區金礦床的成因比較復雜,石英脈+蝕變巖型金礦屬于熱液疊加復合成因礦床,含炭火山碎屑巖型金礦屬於火山沉積?變質熱液改造型層控金礦床。On the basis of this, the paper specially discusses the ore precipitating mechanism and the ore origin. fluid - inclusion observations and microthermometric data suggest that the ore - forming fluid is middle - low temperature hydrothermal solution, it also reports the presence of high - salinity inclusions containing hilite in porphyry rock and ore - hosted quartz vein
流體包裹體巖相學和顯微測溫學研究表明,銀山礦床成礦流體屬于中低溫熱液范疇,在石英斑巖和多金屬礦脈中都發現有含石鹽子礦物的高鹽度流體包裹體。2. considerable progress has been made in the study of ore - forming fluids
對該區與成礦有密切關系的脈石英進行了成礦流體方面的研究。Coal, iron, limestone, dolostone, vein quartz and water resources reach better complementary ; nonmetal ores have abundant reserves and distribute in flakes centralized ; cross railway, network of highways, network circuit in the district, offer the advantage to concentrate on exploitation and transportation and processing
煤、鐵、石灰巖、白雲巖、脈石英等礦產資源與水資源達到了較好的配套程度;非金屬礦儲量豐富,分佈連片集中;區內鐵路、公路網、電路網路縱橫交錯,為礦產資源的集中開采、運輸、加工提供了有利條件。Log ( fh2o / fhcl ) fluid and log ( fhf / fhcl ) fluid ), tongchang porphyry copper deposit system is enriched in chlorine, however dajishan tungsten deposit system is relatively enriched in fluorine, which transport w, sn, nb, ta, et al. ( 8 ) according to the characters of the porphyry copper deposits, copper is transported by chlorine, such as cucl0 and cucl2
忍l ) flu , d 、 109 ( / hr州el ) fluid )發現,銅廠斑巖型銅礦床的成礦體系是相對富氯體系,而大吉山石英脈型鎢礦床成礦體系相對富氟,同時氟可能主要遷移w 、 sn 、 nb 、 ta等金屬元素。Gold deposits are mainly the type of quart vein and etach rock, there are some type of porphyry and scraping rock containing charcoal
金礦以石英脈+蝕變巖型為主,也有含炭碎屑巖型和斑巖型。分享友人