熔析銅 的英文怎麼說

中文拼音 [róngtóng]
熔析銅 英文
liquated copper
  • : 動詞(熔化) melt; fuse; smelt
  • : Ⅰ動詞1. (分開; 散開) divide; separate 2. (分析) analyse; dissect; resolve Ⅱ名詞(姓氏) a surname
  • : 名詞(金屬元素) copper (cu)
  1. The compositions of usual elements and rare earth elements and inclusions of corundum megacrysts related to alkali basalt in changle, shandong province, are analyzed. in the main parts of corundum megacrysts are a large number of fluid - melting inclusions, zircon, ta - columbite inclusions, and in the central crystal core are a large number of melting inclusions. the corundum megacrysts were formed in different periods and different physical chemistry conditions. the crystal core was formed in magma system, and the main parts were formed in inhomogeneously geochemical conditions in which magam and fluid phases coexisted

    山東昌樂與堿性玄武巖有關的剛玉巨晶不同部位的常量元素、稀土元素及包裹體組成.剛玉巨晶的主體以大量流體?體包裹體、鋯石、鈮(鉭)鐵礦包裹體為主,而巨晶中的「晶核」部位則以大量的體包裹體為主,反映研究區的剛玉巨晶是在不同的階段形成的.剛玉「晶核」以及「皮剛玉」形成於體相為主的體系中,而主體剛玉則形成於體?流體過渡的急劇變化的不均一的地球化學環境中
  2. And apatite. by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china, the characteristics of the granite in this area are concluded as follows. it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p. re congenetic ; the range of temperature is about 500 - 700, the range of pressure is about 2. 50 gpa - 4. 35 gpa, and the range of oxygen fugacity ( lg fo2 ) is - 15. 53 - - 14. 00 ; most granite bodies formed before the collision of plates, and few formed after the collision of plates

    通過對測試數據的分與綜合研究,並同中國和世界一般花崗巖類以及中國主要金、成礦巖體的花崗巖類進行對比,得出本區花崗巖類巖石具有以下特徵:屬磁鐵礦-型或同型花崗巖,其巖漿物質具殼幔混源特徵:主要由融態巖漿經結晶分異作用,通過多期變速上侵而形成;其分異演化程度較低;寄主巖基和包體具有同源性;巖石的形成溫度范圍約為500 - 700 ,壓力大約為2 . 50gpa - 4 . 35gpa ,氧逸度值1gfo _ 2為- 15 . 53 ? 14 . 00 ;該巖帶主要形成於板塊碰撞前消減的活動板塊邊緣期,為燕山至喜馬拉雅早期的大陸邊緣火山弧環境的產物。
  3. The paper discusses dynamical conditions of the supercritical ore - forming fluid system based on study of regional geological background and analyses of physiochemical conditions of ore - forming process and puts forth the ore - forming mechanism : upper mantle uplift - mingling of meteoric water and magmatic hydrothermal fluid separated from acidic magma under tensile or transitional tensile environment - water / rock reaction - transportation - chemical coupling ore precipitation

    在分超臨界成礦流體系統形成的區域地質背景和研究成礦物理化學條件的基礎上,探討了超臨界成礦流體系統形成的動力學條件,提出該系統的成礦機理:與燕山晚期酸性火山侵入巖漿有關的金礦床是在上地慢隆起、張性或向張性過渡背景下形成的,酸性巖漿經體流體分離作用形成的巖漿熱液與大氣降水混合,經水巖作用等復雜的輸運和化學反應耦合過程的動力學產物。
  4. In this paper, the microstructures of the joints of aluminum - bronze surfacing on mild steel and on stainless steel are analyzed by means of sem, and the division and formation of bronze / steel joint bond are studied

    藉助于電子顯微鏡技術對在低碳鋼和不銹鋼上堆焊鋁青的接頭的組織進行了分,並對鋁青接頭合區的形成和區域劃分進行了探討
  5. Abstract : in this paper, the microstructures of the joints of aluminum - bronze surfacing on mild steel and on stainless steel are analyzed by means of sem, and the division and formation of bronze / steel joint bond are studied

    文摘:藉助于電子顯微鏡技術對在低碳鋼和不銹鋼上堆焊鋁青的接頭的組織進行了分,並對鋁青接頭合區的形成和區域劃分進行了探討
  6. Methods for chemical analysis of copper - chromium - zirconium alloys. the determination of zinconium by arsenazo photometric method after fuse with potassium phrosuifate

    鉻鋯合金化學分方法.焦硫酸鉀融?偶氮胂光度法測定鋯
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