褐鐵礦化 的英文怎麼說

中文拼音 [tiěkuànghuà]
褐鐵礦化 英文
ferritization
  • : Ⅰ名 [書面語] (粗布或粗布衣服) coarse cloth or clothingⅡ形容詞(像生栗子皮那樣的顏色) brown
  • : 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
  • 礦化 : mineralize; mineralization礦化帶 mineralized zone; 礦化水 mineralized water
  1. 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

    石為典型少硫物型,金屬物含量極少( 1 - 2 ) ,主要有黃、黃銅和自然金、銀金等。主要脈石物有玉髓、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,屬典型低溫物組合。
  2. 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為主,且重點應在50 - 85度方向糜棱巖、碎裂巖帶中尋找含硫物的石英-方解石脈。
  3. Sulfidizing flotation tests of cerusite and limonite

    的硫浮選試驗研究
  4. 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

    周圍床的風蝕變為表生水提供了質,形成弱酸性的含fe ( oh ) _ 3膠體的水溶液,表生水流經翡翠石時, fe ( oh ) _ 3膠體附著在巖石的表面,經過脫水結晶和吸附,形成膠體,膠體沿裂隙或鬆散的物顆粒進入翡翠巖石中,逐漸累積沉澱,形成次生色層。
  5. The contents of organic material, limonite and manganese hydroxides influence the variation of ore element.

    有機物、和氧錳的含量影響著成元素含量的變異。
  6. The wall rock of ore - bodies is the siliceous dolostone and alkaline volcanic rock ( trachy andesite ) in the yinachang deposit. based on the shape of ore - bodies and the structure and texture of ores, the deposit was identificed as synsedimentary with wall rocks. there occurred ree minerals, such as bastnaesite, monazite and allanite, associated with apatite and fluorite with ree contents to a certain extent

    體產出形態和石的結構構造等均顯示體與賦地層同沉積特徵;出現獨立物氟碳鈰、獨居石及簾石,磷灰石、螢石、菱物中也含有一定量的稀土,沿體走向和垂向稀土元素變不大。
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