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液态不混溶
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  liquid immiscibility
     This experimental study demonstrated that the granite-KBF4-Na2MoO4 system is homogeneous at 1250℃ (105 Pa), which through liquid immiscibility at 1000℃ decomposed in three melts: relative acid globe, relative basic melt and ore-forming melt.
     本文的实验研究表明:1250℃(105Pa)条件下呈均一状态的花岗岩-KBF4-Na2MoO4体系,在1000℃条件下发生液态不混溶形成三种熔体:相对偏酸性的液滴、相对偏基性的熔体和成矿熔体。
短句来源
     The Experimental Study About The Liquid Immiscibility and Ore-Forming process In Felsic Magma
     长英质岩浆中液态不混溶与成矿作用关系的实验研究
短句来源
     This implies that the liquid immiscibility in felsic magma can directly induce the formation of porphery deposit.
     这意味着长英质岩浆中的液态不混溶可直接导致斑岩矿床的形成。
短句来源
     SILICATE MELT TEXTURE AND LIQUID IMMISCIBILITY
     硅酸盐熔体结构与岩浆液态不混溶作用
短句来源
     1. The mineralization of Jiajika, Ke'eryin and Danba deposits respectivelybelong to “magma liquid immiscibility”, “magma fractional crystallization” and“magmatism+metamorphism”.
     1.系统地研究了甲基卡矿床、可尔因矿床和丹巴矿床,认为三者的成因分别属于“岩浆液态不混溶”、“岩浆结晶分异”和“岩浆+变质混合型”。
短句来源
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  “液态不混溶”译为未确定词的双语例句
     The melt structures of the above three immiscible melts mainly differ in the number of bridge oxygen: the highest in the relative acid globe and lower in the relative basic melt, but in the melt structure of the ore-forming melt all oxygen is non-bridge oxygen.
     液态不混溶作用产生的三种不混溶熔体的结构差异明显,主要表现在结构单元中桥氧数目的变化,相对偏酸性的A类小球体的结构单元中桥氧数最高,基底玻璃熔体中桥氧数则相对较少,而成矿熔体中不存在桥氧。
短句来源
     Especially, the continuous immiscible separation in granitoid porphyry magma emplacement formed Au deposits of ore magma, hydrothermal porphyry type and deuteric, hydrothermal turbidite type a`nd corresponding wallrock alteration.
     特别是花岗岩类斑岩岩浆在侵位过程中 ,通过不断的液态不混溶或液态分离演变 ,相继形成斑岩矿浆型、岩浆后期热液成因的斑岩型及以浊积岩为主岩的岩浆后期至岩浆期后热液型金矿体 (床 )和相应的热液蚀变 ,构成较复杂的热液蚀变及成矿系列。
短句来源
     Fluid Immiscibility as a Mechanism of Ore forming Process: the Gold Deposits in the Taihan Mountains as an Example
     液态不混溶作用:成矿机制之一 ——以太行山地区的金矿为例
短句来源
     The Fanshan phosphorus-rich magma experienced unmixing and hence produced three sorts of immiscible liquids:pyroxenitic magma, syenitic magma and phosphate melt.
     矾山岩浆液态不混溶,产生互不混溶的三液相,即辉石质岩浆、正长质岩浆和磷酸盐液相(矿浆)。
短句来源
     On the basisof related thermodynamic model of melt, the reasonable calculation models was estabilished. The latestresults of thermodynamic determination of melts are fully utilized. Through the comparison of chemicalpotential of oxides between the immiscible phases, the immiscibility of the second intrusive stage meltsis proved under the following condition: t=1600~1650℃, p=(8.2~8.5)·10~8 Pa.
     该文在有关溶浆热力学模型基础上建立了合理可行的计算模型,利用熔浆热力学数据测定的最新成果,通过不混溶相化学位的对比,证明在1600~1650℃、压力小于8.2~8.7×1O~8Pa条件下第二侵入期岩浆将发生液态不混溶
短句来源
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  相似匹配句对
     SILICATE MELT TEXTURE AND LIQUID IMMISCIBILITY
     硅酸盐熔体结构与岩浆液态不混溶作用
短句来源
     The Experimental Study About The Liquid Immiscibility and Ore-Forming process In Felsic Magma
     长英质岩浆中液态不混溶与成矿作用关系的实验研究
短句来源
     Stimulated Raman scattering in liquid air
     液态空气的受激喇曼散射
短句来源
     Preparation and application of new liquid photoresist
     新型液态光致抗蚀剂
短句来源
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  liquid immiscibility
Liquid Immiscibility Phenomena in Melts of the ZrO2-FeO-Fe2O3 System
      
This character of the crystallization confirms the presence of the phase separation (liquid immiscibility) region in melts of this system.
      
The possible role of liquid immiscibility of sulfide magma in the development of the mineralogical and geochemical zoning of massive ore is discussed.
      
Liquid immiscibility was detected in aluminous nepheline-and quartz-normative Li-bearing compositions (the latter compositions are characterized by a wider immiscibility field).
      
The fluid-assisted layering of mafic-ultramafic massifs resulted in the contrasting distribution of PGM in response to uneven distribution of sulfur (as well as As, Te, and Bi) during liquid immiscibility.
      
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Six types of igneous rock fragments were distinguished from two polished grain mounts of 250~500 micron soil particles ( 24088, 14 and 24105, 15) . The petrological characteristics are displayed by a progressive variation in rock types from Mg-rich olivine-gabbro to olivine-gabbro, and to ferrogabbro as well as quartz-ferrotroctolite.Basaltic olivines and pyroxenes also exhibit a Fe-rich trend which is consistent with the trend in petrology. According to calculations of fractionation, olivine -gabbro may represent...

Six types of igneous rock fragments were distinguished from two polished grain mounts of 250~500 micron soil particles ( 24088, 14 and 24105, 15) . The petrological characteristics are displayed by a progressive variation in rock types from Mg-rich olivine-gabbro to olivine-gabbro, and to ferrogabbro as well as quartz-ferrotroctolite.Basaltic olivines and pyroxenes also exhibit a Fe-rich trend which is consistent with the trend in petrology. According to calculations of fractionation, olivine -gabbro may represent the parent magma from which the ferrogabbro was derived. The chemical composition of olivine-gabbro is the same as the average composition of Luna 24 basalts and green volcanic glasses. The quartz-ferrotroctolite is the first reported occurrence of this coarse -grained mineral assemblage as a distinct rock fragment. It is considered to be a crystal-line product from a Fe-rich melt containing phosphate, and this melt has under-gone fractional crystallization and silicate liquid immiscibility at the late stage.

在Crisium月海,Luna24登月点,24088,14及24105,15两个土壤碎屑抛光薄片中共辨认出6种火成岩的岩石类型。在粗粒玄武岩(辉长岩)碎屑中,自富镁橄榄辉长岩、橄榄辉长岩、橄长岩至富铁石英橄长岩形成了自富Mg、Cr至富Fe、Ti的岩石演化系列,上述演化趋势与橄榄石、辉石在相应岩石中的变异趋势相吻合。据分离结晶计算结果及岩石结构表明,橄榄辉长岩中含Mg较高者为演化系列的母岩浆,它的化学成分与Luna 24中玄武岩的平均成分以及绿色火成玻璃相当。富镁橄榄辉长岩为其早期的分离结晶物。富铁石英橄长岩为本次工作中发现的一种粗粒火成岩碎屑,它是演化系列最末端的产物,是由铁质辉长岩经分离64%的辉石、20%的斜长石、85%的铁橄榄石后又遭受了液态不混溶作用形成的含P富Fe的熔体结晶的产物。研究表明,Luna24的玄武岩母岩浆可能存在两种以上。

Meishan iron ore deposit is situated at the suburb of Nanjing. Here a block of magnetite is seen intruding between a subvolcanic andesite and a pyroxene amphibole porphyrite. They are cretaceous in age. The contact between the iron ore and the igneous rocks is mainly sharp and clear, without graduaton. The main mineral association of the ore is apatite-diopside-magnetite and the igneous rocks are more or less alkaline.

根据宁芜地区梅山铁矿的地质条件为背景而设计的方铁矿(Wü)-磷灰石(Ap)透辉石(Di)-霞石(Ne)四元系,经1400℃的高温实验,产生了液态不混溶产物——铁浆相和硅酸盐浆相。经电子探针成分分析发现,铁浆相中除主要成分为FeO外,还含有一定数量的硅酸盐、磷酸盐等成分,这些成分含量的多少,是液态不混溶作用发育程度不同的结果。通过可能形成梅山铁矿3种主要矿石类型的平衡反应式,计算了从400℃至1400℃时的lgfo_2值和lgk_T值,并得出梅山铁矿矿浆成矿的结论。

On the basis of detailed reserch on petroilogy, thermodynamics and structure ofmelts, thethree lithofacies of the second stage of Huangshan complex arc considered as theresult of immiscibility of magma.The three lithofacies: olivinfels, Pyroxenolite and gabbrowere formed by threerelevent magma. The changes of lithological characters in everylithofacies were controlled by fractional crystallization.This paper demonstates the abovementioned points of view only on the basis of petrological study.

经过岩石学、热力学及熔体结构等方面的详细研究。笔者认为黄山杂岩体第二侵入体的3个岩相带是岩浆液态不混溶作用的结果。3个岩相带(橄榄岩相、二辉岩相、辉长岩相)分别由相应的3种岩浆形成,岩相内部的岩性变化则是分离结晶作用的结果。该文仅从岩石学角度对上述观点进行论证。

 
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