黃鐵礦礦床 的英文怎麼說

中文拼音 [huángtiěkuàngkuàngchuáng]
黃鐵礦礦床 英文
pyrite deposit
  • : Ⅰ形容詞(像絲瓜花或向日葵花的顏色) yellow Ⅱ名詞1 (指黃河)short for the huanghe river:黃泛區the...
  • : 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...
  • : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
  • : i 名1 (供人睡覺的傢具) bed; couch 2 (像床的器具、地面) something shaped like a bed Ⅱ量詞(用...
  • 鐵礦 : iron ore; plumboniobite; iron mine
  • 礦床 : [地質學] mineral deposit; ore deposit; deposit; mine
  1. 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

    物組成較簡單,金屬物以為主,其次為,有一定量的自然金;脈石物以石英、長石、碳酸鹽為主。
  2. And we compared these deposits for the geological feature and the typmorphic feature of pyrite, galenite, shphalerite which provide mineral basis for prospective value and reserching target of these deposits

    而且把幾個的地質特徵以及、方鉛、閃鋅的標型特徵進行對比,為區的遠景評價和找靶區的確定提供了物學依據。
  3. That offer very valuable referential material for future searching mineral. in recent years, many deposits were confronted with reserves crisis in yuebei region. so we studied the typomorphic feature of pyrites, galenite, sphalerite for deposit of yuebei region, and sum up the genesis of deposit and mineral and reseaching typmorphic feature, these have important value to forecast the deepth of deposit and reaserch the outside of deposit

    近幾年,粵北地區的許多面臨儲量危機,因而對粵北地區、方鉛、閃鋅的標型特徵進行研究,總結出凡口、紅巖、大寶山等物的成因和找標型特徵,對于進行的深部預測和外圍找工作具有十分重要的意義。
  4. Xiongcun copper - gold ore deposit is located in gangdese metallogenetic belt with a large scale. the ore body mainly exists in the second lithoid unit ' s tuffs and the third lithoid unit ' s dacite tufa of the cretaceous volcanic stratum, which are not only mother rock but also mineralized body

    雄村銅金處于岡底斯成帶,規模巨大,體主要賦存於白堊系火山巖地層第二巖性單元的絹英巖化硅化凝灰巖和第三巖性單元英安質疑灰巖中,上述巖石既是賦圍巖又是化體。
  5. Study on mineralogical characteristic of pyrite in huang - sha gold deposition of jiangxi

    江西沙金物學特徵研究
  6. Reconnessance investigation of pyrrhotite in dongshan iron deposit of nanshan iron mine

    南山東山的普查研究
  7. This paper has described relative information of gold depositions genesis and hunting besed on studying characteristic of occurrence and appearance, compositions of trace elements, cell parameters, thermoelectricity, ir spectroscope with pyrite in huang - sha gold depositon of jiangxi. it can be provided important scientific basis for evaluation this deposition and hunting a similar ore point or zone in huang - sha region

    通過對江西沙金的產狀及形態特徵、成分特徵、晶胞參數特徵、熱電性、紅外光譜特徵等物學的詳細研究,討論了中蘊藏的金成因及找信息,為正確評價該和在該區找尋新的金點(帶)提供了重要的依據。
  8. The ore - bearing fluid of dabaoshan deposit was relate to magmatic thermal dynamic process and formed hydrothermal sedimentary polymetallic deposit at seafloor. the ore - bearing fluid of fankou was relate to circulation hydrothermal fluid in deep formation and formed pb - zn - ag - hg polymetallic middle - lower temperature sedimentary deposit by sea - floor thermal spring overflowing

    大寶山型流體與巖漿熱動力作用有關,形成海底火山熱液沉積多金屬;凡口型流體與深部建造的循環熱液有關,形成中低溫海底熱泉噴溢沉積鉛鋅銀汞;紅巖型流體與盆地成巖壓實水有關,形成低溫單一黃鐵礦礦床
  9. 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

    通過對大寶山的成地質背景、物成分、稀土元素組成、同位素以及、閃鋅、方鉛的標型特徵進行研究,確定了大寶山的成因為火山沉積,經後期巖漿熱液疊加型,對的遠景進行了預測,提出大寶山的上部體已被剝蝕或被氧化,基本上已經到體的深部的觀點。
  10. We forecasted that the deposit was very prospective yet by study the thermoelectric feature of pyrite and supposing the deepth of the deposit, and that have been proved by practice

    並且通過的熱電性對進行了深部預測,說明具有很好的找遠景,已經得到實踐檢驗。
  11. According to tectono - metallogenic setting in combination with main mineral distribution and metallogenic types and ore - forming epochs in this orogenic belt, the authors used the theory of metallogenic series to divide the deposits of the north qilian early palaeozoic convergent epicontinental cu, pd, zn, w ( mo ), au, ophiolite metallogenic belt and the south qilian early palaeozoic epicontinental rifting cu, ni ( pt ), cr, au, rare elements and pyrite metallogenic belt into six series

    文章依據成構造環境,結合區域主要種分佈及其成類型和成時代等特徵,應用系列理論,將祁連造山帶北祁連早古生代匯聚陸緣銅、鉛、鋅、鎢(鉬) 、金、蛇蚊石成帶和南祁連早古生代陸緣裂解帶銅、鎳(鉑族) 、鉻、金、稀土、帶中的劃歸為6個成系列。
  12. By analyzing and generalizing minerogenetic and geological background, mineral constituent, rare - earth element, isotope and typomorphic feature of sulpurization mineral, finally, we made a conclusion that fankou desposit resulted from the hot spring eruption at the bottom of sea, it has a character of syngenetic sedimentary deposit, which was affected by the late hydrothermal superimposed and light rebuilding after it came into being, which is typical sedex bedded - controlled deposit

    通過對凡口的成地質背景、物成分、稀土元素、同位素以及的、閃鋅、方鉛標型特徵進行了分析總結,確定了凡口是海底熱泉噴溢形成的,同時又受到後期熱液輕微疊加改造,屬于典型的sedex型層控
  13. Pyritic bedded deposit

    層狀
  14. Warmhearted water deposited eruption of sea floor pyrite rolled cakes have been discovered, in the layers of 1a, 1b, 1c and so on. some warmhearted water deposited feature mineral could been seen under the microscope, such as tourmaline ect. warmhearted water deposited eruption of early phase pyrite ' s rolled cakes is one of gold mine bed mine source

    在1a 、 1b 、 1c等地層中,可發現海底熱水沉積所噴發的團塊,在顯微鏡下可以看到一些熱水沉積的特徵物,如電氣石等,早期熱水沉積所噴發的團塊為金源之一。
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