鋅鉛中礦 的英文怎麼說

中文拼音 [xīnqiānzhōngkuàng]
鋅鉛中礦 英文
zinc and lead middlings
  • 鋅 : 名詞[化學] （金屬元素） zinc （zn）
  • 鉛 : 鉛名詞1. （金屬元素） lead （pb） 2. （鉛筆心） lead （in a pencil）; black lead
  • 礦 : 名詞1. （礦床） ore [mineral] deposit 2. （礦石） ore 3. （開采礦物的場所） mine
  1. The main metals mineral are chalcopyrite, the next clinohedrite, alpha chalcocite bornite, malachite and azurite. a little amount blende, galena incidentally ryby silver, bismuth

    礦石中主要金屬礦物為黃銅礦、其次為黝銅礦、蘭輝銅礦、斑銅礦及銅的氧化物孔雀石、藍銅礦。閃鋅礦、方鉛礦少量，偶見淡紅銀礦、硫酸鈕礦。
  2. Flotation technique for a hard - to - separate copper sulphide mine

    從凡口鉛鋅礦尾礦中回收硫精礦的研究
  3. 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。
  4. Germanium enriched mainly in galenite, and cadmium enriched mainly in nonage sphalerite ; isomorphism is the subsistent state of ge and cd, but it ca n ' t exclude the probability that ge and cd absorbed by organic matter

    Ge主要富集在方鉛礦中， cd主要富集於早期閃鋅礦中； ge 、 cd的賦存狀態為類質同象，但不排除部分被有機質吸附的可能性。
  5. The ore minerals are mainly composed of marmatlte, galenit, pyrrhotite ( pyrite ), chalcopyrite, or marmatite, galenite, pyrite and hedenbergite. marmatite and hedenbergite are the indicated minerals of the ore

    主要礦物組合為鐵閃鋅礦-方鉛礦-磁黃鐵礦（黃鐵礦） -黃銅礦或鐵閃鋅礦-方鉛礦-黃鐵礦-鈣鐵輝石，其中鐵閃鋅礦和鈣鐵輝石為該類礦石標型礦物。
  6. Simultaneous determination of six metal elements of micro - amounts in pure p - phthalic acid by icp - aes

    法測定銀精礦中銀銅鉛鋅砷
  7. And some fabulous new samples of green fluorite on sphalerite and galena from naica, mexico, which were collected some time this year - here evan is holding one of the best examples of this new find

    還有一些新標本的如來自於墨西哥奈卡的閃鋅礦和方鉛礦上共生綠色螢石，這是今年的熱門收藏，埃文在此次展會上最好的一批中淘到了一個。
  8. The weishan - yongping copper - gold - polymetallic mineralization district in yunnan is tectonically located in the southern part of lanping basin in the middle part of changdu - simao block between lanchangjiang fault and jinshajiang - ailaoshan fault. more than 140 deposits and occurrences of gold, copper ( cobalt ), stibium, mercury, lead, zinc, iron etc. have been found in the area studied, and there are 4 medium - sized deposits among them

    雲南巍山-永平銅金多金屬礦化集中區位於瀾滄江大斷裂與金沙江大斷裂、哀牢山大斷裂之間的昌都-思茅中間地塊中部的蘭坪盆地的南段，礦化集中區內目前已發現金、銅（鈷） 、銻、汞、鉛、鋅、鐵等各種金屬礦床（點） 140處，其中達中型規模的礦床有4個。
  9. A comparison of the prospecting model of the hf type with the prediction model of the vms type reveals that their thermal dynamic mechanisms are different : the former is related to basic - ultrabasic rock intrusion, while the latter to acidic rock intrusion

    與白銀銅礦區域地球化學預測模式相比較，富鐵型鉛鋅礦床中除鐵族元素指示基性超基性巖侵入事件外，其他元素均大致相似，兩大類礦床形成的初始熱動力條件不同。
  10. There are a series of lead - zinc polymetallic deposits, such as fozichong, dongtao, xiashui, wenlongjing and jilongding distributed along the fault zone. these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore. these deposits may be included in the same metallogenic series

    佛子沖、東桃、下水、文龍徑、雞籠頂等一系列鉛鋅多金屬礦床沿該斷裂帶分佈，這些礦床雖然在成礦規模、賦礦層位和礦石礦物組成等方面存在一些差異，但均產于下古生界地層中；主要礦體呈層狀、似層狀產出，與地層產狀大體一致；直接賦礦圍巖為層狀綠色巖或重晶石巖；礦石中保留有典型的同生沉積組構。
  11. The minesoils possessed obviously different mciobial features : higher in microbial basal respiration strength, and microbial ecophysiological parameters cmic / corg and qco2, but lower in micobial biomass compared with the non - minesoils. biolog data showed that were changed, much more rapid in consuming carbon sources, but the lower in the ratio of utilization

    結果表明：香根草是一種在鉛鋅礦區適生的耐受性植物，引種5年以上的香根草植物中元素含量表現為zn pb cu cd ，其中cu表現為根莖葉， cd表現為葉莖根， zn 、 pb表現為根葉莖。
  12. Thermal deposits mainly formed during middle - late yanshanian age, related to extension structure, with main mineralization in qingfeng competent deformation zone, western shennongjia fault arch, northern huangling fault arch, xianfeng anticline of enshi platforman fold bundle

    熱液型鉛鋅礦床主要形成燕山中晚期，與滑脫拆離構造密切相關，礦化主要集中於青峰強變形帶、神農架斷穹西部、黃陵斷穹北部、恩施褶皺束咸豐背斜、長陽褶皺束走馬坪背斜中。
  13. 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。
  14. In order to choose the plants that were hypertolerant to heavy metals and for the case of phytoremediation of soils that were polluted by heavy metals, the research was carried out by the methods of soil - planting and sand - planting in green - house. the study includes selecting the hypertolerant plants from 36 dominant species found in the vicinity of a pb / zn mine tailings pond, observing the ecophysiological response of the hyperaccumulators, improving - impact of hyperaccumulators on biosolds and examining the effect of nutrient elements ( n p k ) on the lead uptake

    為選擇和篩選富集重金屬或對重金屬具有耐性的植物，以達到利用植物修復重金屬污染土壤的目的，本研究通過溫室砂培和土培的方法，對生長于鉛鋅尾礦區的36種植物進行了篩選，研究了富集植物品種對重金屬pb的生理生態效應、對重金屬pb的吸收和耐性以及對污泥的響應，並探討了土壤中的營養元素n 、 p 、 k對植物吸收pb的影響，為植物修復工作提供理論依據。
  15. There is a close relation between mesozoic tectonic evolution, fluid evolution, petrogenesis and mineralization in the manzhouli - e ' erguna region in the northeast of the northern orogenic belt, china, and three evolution stages of the mesozoic tectonic - fluid - petrogenetic and metallogenetic system are proposed out : 1 ) acompanied by ree and cu mineralization, the calc - alkaline volcanic rocks and mantle - crust mixed type granite occurred under the regional tension tectonic background caused by the mongolia - okhotsk residual ocean that was closing in scissors form in the early - middle jurassic. 2 ) acompanied by pb, zn and ag mineralization, the calc - alkaline and alkaline volcanic rocks occurred under the regional shear - compression tectonic background in the late jurassic. 3 ) acompanied by u, f, pb, zn and ag mineralization, the caic - alkaline and alkaline volcanic rocks occurred under the regional tension tectonic background in the early cretaceous

    摘要本文討論了北方造山帶東北段滿洲里額爾古納地區及其毗鄰區中生代構造流體成巖成礦系統及其演化的三個不同階段： 1 ）早中侏羅世張性「似裂谷環境」下所形成的中基性堿性火山巖、同熔性花崗巖及深源流體活動形成的稀土礦床和斑巖性銅鋁礦床； 2 ）晚侏羅世擠壓剪切環境下所形成的酸性火山巖、斑巖類及深源流體活動所形成的鉛鋅銀礦床； 3 ）早白堊世張性環境下所形成的基性堿性火山巖及深源流體活動所形成的鈾礦床、金銀礦床及螢石礦床。
  16. In the concentrated mineralization area, there are many types of pb - zn - ( ag ) deposits and gold deposits, it is one of bases of lead - zinc in china. in this area seafloor hydrothermal sedimentary ore deposits and hydrothermal sedimentary - rebuilded ore deposits are predominated. all lead - zinc - ( silver ) and gold deposits hosted in devonian sedimentary rocks, and orebodies of seafloor hydrothermal sedimentary deposits and hydrothermal sedimentary - rebuilded deposits draped in phase with stratum

    礦化集中區內主要的礦床類型是熱水沉積型和熱水沉積改造型，其中熱水沉積成礦作用形成的廠壩-李家溝礦床為超大型礦床，熱水沉積-改造型礦床有畢家山和鄧家山等大型鉛鋅（銀）礦床，礦床與中泥盆統地層整合產出，並同步褶曲。
  17. Distribution of anthraxolite and metallogeny of the jinding lead - zinc deposit

    金頂鉛鋅礦床中碳瀝青的分佈特徵及成礦作用
  18. In the main ( no. ) orebody, it is characterized by high as content but low sb, in no. orebody, it is characterized by high sb content but low as ; in both orebodies, it is characterized by high zn content and insignificant temporal and spatial variations of chemical compositions

    在以銅為主的主礦體（號礦體）中，黝銅礦幾乎均屬鋅砷黝銅礦，含銀甚低，其化學成分在時空分佈上變化不大且無顯著的變化規律，不同類型礦石之間黝銅礦的成分變化也不大；但在以鉛鋅為主的次要的號礦體中黝銅礦含一定量的銀。
  19. The ne - trending yiwulushan mountains is located in western liaoning province with the fuxin basin as its western boundary and xialiaohe depression as its eastern boundary. our study area belongs to the fuxin au - concentrating zoning in northeastern part of the yanshan intercontinental orogeny in northern margin of the huabei ( north china ) block, where converge the ew - trending weichang - chifeng - fuxin cu - concentrating zoning in northern yanshan orogeny and the ne - trending suizhong - jinzhou - fuxin au - pb - zn - mo mineralization sequence

    研究區屬華北地塊北緣的燕山陸內造山帶的東北端的阜新金礦集中區，是東西走向的燕山北緣圍場-赤峰-阜新金銀銅成礦帶與北東走向的綏中-錦州-阜新金鉛鋅鉬成礦列的交匯處。
  20. Huize pb - zn - ge - cd deposit is a typical ore deposit occurred in sichuan - yunnan - guizhou lead - zinc metallogenic area. the enrichment coefficient of ge and cd in main ore body reaches 6978 and 3640 respectively, which shows that dispersed elements have a special geochemical behavior in this area

    會澤鉛鋅鍺鎘礦床，是川滇黔成礦三角區富分散元素鉛鋅礦床的典型代表，其主礦體中鍺、鎘的富集系數分別可達6978和3640 ，顯示了分散元素在該區有著獨特的地球化學行為。
分享友人
分享到 Line

分享到臉書