硫礦床 的英文怎麼說
中文拼音 [liúkuàngchuáng]
硫礦床
英文
sulfur deposit-
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
成礦物質主要來自礦區火山巖圍巖,次火山巖提供了主要熱源和部分礦源,成礦流體來自大氣降水,礦床成因類型為低硫化物冰長石?絹雲母型淺成低溫熱液型金礦。Gold ore main type is auriferous quartz vein type
金礦床主要為含金硫化物石英脈型。Trace element geochemistry of cassiterite from the neves corvo massive sulfide deposit, portugal
塊狀硫化物礦床錫石的微量元素地球化學Study of ore compositions in no. 100 orebody of dachang cassiterite - polymetallic sulfide deposit of guangxi
多金屬硫化物礦床100號礦體物質成分研究Geological traits of cassiterite - sulfide deposit of tieshanping at linwu and its significance on exploring deposits
硫化物礦床地質特徵及找礦意義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,佛子沖礦田硫同位素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硫化物礦床的6噸陸值大體一致。In all hydrothermal deposits the minerals formed are not solely the sulfide ore minerals.
在所有熱液礦床中,所形成的礦物並不單單是硫化物礦石礦物。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硫化物礦床的成巖成礦機制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
通過對礦床的常量元素、微量元素、稀土元素、流體包裹體特徵、氫氧同位素、硫同位素、鉛同位素等特徵的研究,認為成礦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,成礦作用有三期,分別與區內的花崗巖、二長花崗巖脈、雲煌巖脈有關。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礦集區的初步研究,發現該區的礦床具有塊狀硫化物礦床的典型特徵,並存在多元礦化的可能。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硫鐵礦礦床外,其他中、小型礦床及礦點更是星羅棋布。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、硫鐵礦等礦床主要分佈在粵北仁化、樂昌、英德等地。Test to distinguish spontaneous fire in sulphide mineral mine
硫化礦床內因火災滅火試驗研究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硫化物礦床的金川巖體相比,煎茶嶺超基性巖體為巖漿一次侵位形成,分異程度小,鎳、硫含量較低。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硫化物巖漿礦床。該類礦床佔世界鎳、鉑量的近一半或更多。The developments of study on ancient and modern volcanogenic massive sulfide deposit
古代與現代火山成因塊狀硫化物礦床研究進展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、輝石等單礦物的原位la ? icp ? ms分析等,在我國還是首次,為研究我國主要銅鎳硫化物礦床成巖成礦過程中元素的分異和演化提供了定量結果。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硫化物礦(床)體。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.長江中下游硫化物礦床氧化帶及鐵帽評價研究[ m ] .北京:地質出版社, 1980The prevention and control on spontaneous combustion of sulfide ores are always the main safety problem for sulfide ore deposits
摘要硫化礦石自燃的防治一直是含硫礦床面對的主要安全問題。分享友人