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- 黃 : 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...
- 鐵 : 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...
- 礦 : 名詞1. (礦床) ore [mineral] deposit 2. (礦石) ore 3. (開采礦物的場所) mine
- 床 : 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
-
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。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
而且把幾個礦床的地質特徵以及黃鐵礦、方鉛礦、閃鋅礦的標型特徵進行對比,為礦區的遠景評價和找礦靶區的確定提供了礦物學依據。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,粵北地區的許多礦床面臨儲量危機,因而對粵北地區礦床黃鐵礦、方鉛礦、閃鋅礦的標型特徵進行研究,總結出凡口、紅巖、大寶山等礦床礦物的成因和找礦標型特徵,對于進行礦床的深部預測和外圍找礦工作具有十分重要的意義。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
雄村銅金礦床處于岡底斯成礦帶,礦床規模巨大,礦體主要賦存於白堊系火山巖地層第二巖性單元的黃鐵絹英巖化硅化凝灰巖和第三巖性單元英安質疑灰巖中,上述巖石既是賦礦圍巖又是礦化體。Study on mineralogical characteristic of pyrite in huang - sha gold deposition of jiangxi
江西黃沙金礦床黃鐵礦礦物學特徵研究Reconnessance investigation of pyrrhotite in dongshan iron deposit of nanshan iron mine
南山鐵礦東山礦床磁黃鐵礦的普查研究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
通過對江西黃沙金礦床中黃鐵礦的產狀及形態特徵、成分特徵、晶胞參數特徵、熱電性、紅外光譜特徵等礦物學的詳細研究,討論了黃沙礦中蘊藏的金礦成因及找礦信息,為正確評價該礦床和在該區找尋新的金礦點(帶)提供了重要的依據。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礦床;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礦床;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。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質背景、礦物成分、稀土元素組成、同位素以及黃鐵礦、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沉積,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。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
並且通過黃鐵礦的熱電性對礦床進行了深部預測,說明礦床具有很好的找礦遠景,已經得到實踐檢驗。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
文章依據成礦構造環境,結合區域主要礦種分佈及其成礦類型和成礦時代等特徵,應用礦床成礦系列理論,將祁連造山帶北祁連早古生代匯聚陸緣銅、鉛、鋅、鎢(鉬) 、金、蛇蚊石成礦帶和南祁連早古生代陸緣裂解帶銅、鎳(鉑族) 、鉻、金、稀土、黃鐵礦成礦帶中的礦床劃歸為6個成礦系列。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
通過對凡口礦床的成礦地質背景、礦物成分、稀土元素、同位素以及的黃鐵礦、閃鋅礦、方鉛礦標型特徵進行了分析總結,確定了凡口礦床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型層控礦床。Pyritic bedded deposit
黃鐵礦層狀礦床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黃鐵礦團塊,在顯微鏡下可以看到一些熱水沉積的特徵礦物,如電氣石等,早期熱水沉積所噴發的黃鐵礦團塊為金礦床礦源之一。分享友人