綠泥 的英文怎麼說

中文拼音 [lǚní]
綠泥 英文
[地質學] green mud綠泥石 chlorite; 綠泥石化 choritization
  • 綠 : 綠形容詞（像草和樹葉茂盛時的顏色） green
  • 泥 : 泥名詞1 （含水的半固體狀的土） mud; mire 2 （像泥的東西） any paste like matter; mashed vegetable...
  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

    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。
  2. Amphibole - cholrite schist

    閃綠泥片巖
  3. Of these minerals, kaolinite, illite and chlorite are commonest.

    在這些礦物中，高嶺石，伊利石和綠泥石最常見。
  4. Glaucophane - chlorite schist

    藍閃綠泥片巖
  5. Epidote - chlorite schist

    綠簾綠泥片巖
  6. Corrensite forms networks of crinkled or folded sheets.

    柯綠泥石呈捲曲網狀或折迭片狀。
  7. The ore ' s mineral component is simple, and its main association of minerals are leucocratic sphalerite - galenite ? iopsite ( epidot, chlorite ). leucoratic sphalerite and diopsite are the guide minerals in the ore

    主要礦物組合為淺色閃鋅礦-方鉛礦-透輝石（綠簾石、綠泥石） ，其中淺色閃鋅礦和透輝石為該類礦石的標型礦物。
  8. Clay fraction is dominated by illite and kaolinite with small proportions of smectite, chlorite and vermiculite

    粘粒組成主要為伊利石和高嶺石，也有少量蒙皂石、綠泥石和蛭石。
  9. The fluids upwelled to seafloor along fault thus ore - forming metals accumulated. 2. this paper indicated the definition the hydrothermal sedimentary rocks. the definition is a group of especial sedimentary rocks forming at the temperature ranging from 70 ? to 350 ? ( or more high ) through sedimentation and synsedimentary metasomatism in the seafloor

    區內的熱水沉積巖主要有硅質巖、鈉鉀長石巖、重晶石巖、透閃石巖、碳酸鹽巖、綠泥石巖和鐵白雲石斑點千枚巖，它們往往與熱水沉積礦體緊密伴生。
  10. In the ranger area highly chloritic rocks were believed to be altered dolerites.

    蘭傑地區的強烈綠泥石化巖石據信可能是蝕變粒玄巖。
  11. Talc - chlorite schist

    滑石綠泥片巖
  12. The hydrothermal activities which were complicated and acted a positive effect in the formation of the zhulazaga gold deposit resulted in hydrothermal alterations of multiepisode, including pyroxeneization, actinolitization, epidotization, ice - feldsparization, silicification, chloritization and carbonatization etc. the research on inclusions in quartz of the ore indicates that the hydrothermal fluid varying greatly in temperature with an average of 286 shows characteristics of high temperature

    3 、朱拉扎嘎金礦的形成中熱液活動起到了積極的作用，熱液活動不僅復雜而且具多期性，有透輝石化、陽起石化、綠簾石化、綠泥石化、硅化、冰長石化、碳酸鹽化等。礦石中石英包裹體的研究表明，含礦熱液的溫度變化范圍較寬廣，平均在286 ，顯示中偏高溫特徵。
  13. When applied to the face or body, green clay cleanses, exfoliates, smooths and softens the skin

    綠泥用於皮膚（臉部或身體）有清潔，去死皮，柔滑的功效。
  14. Green clay is the most absorbent of all the clays and is ideal to use in face masks for the treatment of acne, oily and neglected skin

    綠泥是所有泥中吸收力最好的，對粉刺，過油和疏於保養的皮膚是理想的面膜。
  15. The cementation of laumonite, calcite and chlorite, compact and pressure solution, as well as the dissolution of laumontite, feldspar are also of main factors which affect reservoir properties

    方解石、綠泥石、濁沸石的膠結作用、壓實壓溶作用和濁沸石、長石的溶解作用也是影響儲集性能的主要因素。
  16. Clay minerals are of illite, chlorite, kaolinite and smectite assemlblage. the content of illite is very high and its crystallinity index is high too, which indicate the cool and arid climate condition in the time of sediment conformation

    粘土礦物組合為伊利石、綠泥石、高嶺石和蒙皂石，伊利石含量占絕對優勢，其結晶度指數（ hw ）較高，反映東海南部外陸架粘土形成於寒冷乾燥的氣候環境。
  17. Fine - grained feldspar sandstone is the main oil - bearing rock and chlorite is the dominant kind of clay minerals

    研究結果表明，長2油藏含油砂巖以細粒長石砂巖為主，粘土礦物中綠泥石含量較高。
  18. Group leading products for magnesium fertilizer products series, magnesium oxide product series, lingmei chemical products series, lu : nidan powder and powder series

    集團的主導產品為鎂肥料產品系列、氧化鎂產品系列、菱鎂化工產品系列、綠泥石粉及滑石粉系列。
  19. The xrd and sem indicate that the types clay consists of i / s mixed layer, illite and kaolinite. the i / s mixed layer is the most abundant mineral in the clay samples. the chlorite clay mineral has not been detected in the formation

    Xrd與sem綜合分析證實，砂巖中粘土礦物由i s混層、伊利石與高嶺石組成，其中以i s混層為主，樣品中沒有發現綠泥石礦物。
  20. With the intermittent activity of hot fluid containing cc ^, ferrous carbonate minerals dissolved and precipitate repeatedly many times. in addition, dissolution of shells and feldspars, decrease of chlorite and increase of kaolinite could be found

    隨著富co _ 2熱流體多次間歇性入侵導致了含鐵碳酸鹽礦物的反復多次溶解和沉澱、生物介殼大量溶蝕和長石鑄模孔的形成以及綠泥石消失、高嶺石增加等。
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