硫礦床 的英文怎麼說

中文拼音 [liúkuàngchuáng]
硫礦床 英文
sulfur deposit
  • : 名詞[化學] sulphur; sulfur [美國] (16號元素, 符號s)
  • : 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...
  • 礦床 : [地質學] mineral deposit; ore deposit; deposit; mine
  1. The ore - forming material is mostly from volcanic rock, and sub volcanic rock provides the main thermal and some mineral materials. the ore - forming fluid is from meteoric water. as a result, it should be a kind of adularia - sericite type of epithermal gold deposit

    物質主要來自區火山巖圍巖,次火山巖提供了主要熱源和部分源,成流體來自大氣降水,成因類型為低化物冰長石?絹雲母型淺成低溫熱液型金
  2. Gold ore main type is auriferous quartz vein type

    主要為含金化物石英脈型。
  3. Trace element geochemistry of cassiterite from the neves corvo massive sulfide deposit, portugal

    塊狀化物錫石的微量元素地球化學
  4. Study of ore compositions in no. 100 orebody of dachang cassiterite - polymetallic sulfide deposit of guangxi

    多金屬化物100號體物質成分研究
  5. Geological traits of cassiterite - sulfide deposit of tieshanping at linwu and its significance on exploring deposits

    化物地質特徵及找意義
  6. In terms of sulphur isotope result from sphalerite, galenite > pyrite and chalcopyrite, the 8 34s % o value obtained in fozichong orefield ranges mainly between 0 ~ + 5, which is coincident with the average 5 34s % o value of submarine stratabound sulphide deposits in silurian strate distributed over other areas of the world

    地球化學研究顯示,佛子沖同位素5倫值主要集中分佈在0 5之間,與世界其它地區志留系海相化物的6噸陸值大體一致。
  7. In all hydrothermal deposits the minerals formed are not solely the sulfide ore minerals.

    在所有熱液中,所形成的物並不單單是化物物。
  8. Geochemical characters of mafic - ultramafic swarms in the baimazhai nickel and copper deposit, jinping, yunnan

    超鎂鐵巖侵入體及銅鎳化物的成巖成機制
  9. Through the study of characteristic of macroelement, microelement, rare - earth element, oxyhydrogen isotope, sulfur isotope, lead isotope, fluid inclusion etc, a conclusion can be drawn that metallogenic substance comes from the upper mantle with mixing of some substance from the upper crust latter. it is likely to have the same source with the surrounding rock

    通過對的常量元素、微量元素、稀土元素、流體包裹體特徵、氫氧同位素、同位素、鉛同位素等特徵的研究,認為成物質主要來源於上地幔,與周圍巖石存在著同源的可能性,後期有一定的上地殼物質混入,成作用有三期,分別與區內的花崗巖、二長花崗巖脈、雲煌巖脈有關。
  10. But through our research on the hetaoping mineralization - concentrated region, we find that the deposits in this area have a lot of typical characteristics of massive sulfide deposits, and it also has the possibility of polygenesis

    最近,通過對保山北部核桃坪集區的初步研究,發現該區的具有塊狀化物的典型特徵,並存在多元化的可能。
  11. Besides fankou, dabaoshan and yingde are known large non - ferrous metal and pyrite bed, other medium and small scale deposits and mineralized spots scatter everywhere. these depositsmostlty exist in the middle - late devonian strata, others exist in carboniferrous

    除著名的凡口、大寶山以及英德等幾個大型有色金屬及外,其他中、小型點更是星羅棋布。
  12. The deposit such as copper, lead, zinc, mercury, stibium, pyrite spread aroud renhua of yuebei, lechang, yingde and so on

    銅、鉛、鋅、汞、銻、主要分佈在粵北仁化、樂昌、英德等地。
  13. Test to distinguish spontaneous fire in sulphide mineral mine

    內因火災滅火試驗研究
  14. However, compared with jinchuan ore - bearing intrusion, jianchaling ultrabasic intrusion formed by magma simple emplacement, and magma fractionated weakly with lower content of nickel and sulphur

    而與賦存超大型鎳銅化物的金川巖體相比,煎茶嶺超基性巖體為巖漿一次侵位形成,分異程度小,鎳、含量較低。
  15. The main source of nickel and platinum metals in the world is the nickel - copper sulfide magmatic deposits related to basic - ultrabasic body, which provide half or more amount of the metals in the world

    世界鎳和鉑族金屬的主要來源是與基性超基性巖有關的銅鎳化物巖漿。該類佔世界鎳、鉑量的近一半或更多。
  16. The developments of study on ancient and modern volcanogenic massive sulfide deposit

    古代與現代火山成因塊狀化物研究進展
  17. Systematically tested, analyzed and sorted out geochemical data of intrusion - related nickel deposits in china, such as analysis of zonal structure of chrome spinels, micro - probe in situ analysis of single minerals incjude olivine and pyroxene by la - icp - ms, in which some of the research is the first time domestically

    其中一些研究,如鉻尖晶石環帶的研究、橄欖石、輝石等單物的原位la ? icp ? ms分析等,在我國還是首次,為研究我國主要銅鎳化物成巖成過程中元素的分異和演化提供了定量結果。
  18. There are over 30 mafic and ultramafic intrusions in the area and cu - ni sulfide ore bodies were found in no. 1 and no. 7 ultramafic intrusive bodies which exhibit obvious zoning and cumulate texture

    區內出露30多個鎂鐵超鎂鐵質巖體,其中1 、 7號超鎂鐵巖體中賦存銅鎳化物)體。
  19. Herzig p m, hnnington m d, scott s d, et al. gold - rich sea - floor gossans in the troodos ophiolite and on the mid - altantic ridge [ j ]. economic geology, 1991, 36 : 1747

    李文達,王文斌,孫南圭,等.長江中下游化物氧化帶及鐵帽評價研究[ m ] .北京:地質出版社, 1980
  20. The prevention and control on spontaneous combustion of sulfide ores are always the main safety problem for sulfide ore deposits

    摘要石自燃的防治一直是含硫礦床面對的主要安全問題。
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