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化学差异
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  “化学差异”译为未确定词的双语例句
     Intrusive rocks of the two series show systematic chemical differences, and generally experienced fractional crystallization of mafic minerals at the high magmatic chamber.
     这两个系列的侵入岩存在系统的化学差异,而且在高位岩浆房中普遍经历了镁铁矿物的分离结晶作用。
短句来源
     The chemical differences between these two series resulted from the higher melting degree of the tholeiite series than that of the calc-alkaline series.
     两个系列间的化学差异起因于拉斑系列的熔融程度高于钙碱系列。
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  相似匹配句对
     Results There was significance difference in size of SPT between Alutard and existing Chinese allergens.
     的差异 .
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     The Difference
     差异
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     Study on the Differences of Chemistry Characteristics of Luzhou Laojiao Daqu
     泸州老窖大曲化学特性差异研究
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     CHAPTER 5 MARINE SEDIMENTATION Section 5 Sedimentary Chemistry
     沉积物化学
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     Electroless Copper Plating
     化学镀铜
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  chemical difference
Therefore, the profound chemical difference between proteins and nucleic acids is not an insuperable barrier to their functional interchangeability in certain situations.
      
To avoid such artifacts, oriented unaveraged atomic states must be subtracted for the formation of meaningful Chemical Difference Densities.
      
This chemical difference is assumed to cause the difference in the biological behavior.
      
This chemical difference was utilized for the development of a fluorescence microscopic method for distinction between collagen and elastin.
      
An intrinsic bias in clinical detection was excluded since frequencies of specific amino acid substitutions did not correlate with the 'chemical difference' between the amino acids exchanged.
      
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Migration of Cu and Zn in soils derived from basalt in Zhejiang Province occurs in their soil forming process. The amount of migration of Cu is larger than that of Zn. However,the influence of the migration of these elements on their total contents is less than that of the geochemical difference of parent materials. Cu and Zn contents in the surface soil are higher than those in subsoil, and those in the soils with a higher altitute are higher than those in the soils with a lower altitute. The effect of pH is...

Migration of Cu and Zn in soils derived from basalt in Zhejiang Province occurs in their soil forming process. The amount of migration of Cu is larger than that of Zn. However,the influence of the migration of these elements on their total contents is less than that of the geochemical difference of parent materials. Cu and Zn contents in the surface soil are higher than those in subsoil, and those in the soils with a higher altitute are higher than those in the soils with a lower altitute. The effect of pH is insignificant. The ratio of amorphous Cu to total Cu in the soils with similar allitic process increases with the increase of the altitute at which the soils are located, i.e. there is significant difference in the ratio among the red earths, yellow-red earths and yellow earth. However, the content of amorphous Cu tends to be decreased with the intensification of weathering and eluviation proceses.All these may be used as factors for soil classification and evaluation of soil fertility.

在成土过程中,铜和锌均有移动,迁移量铜大于锌,但这种作用小于母岩地球化学差异对总含量的影响。铜和锌的有效态含量,表土高于底土,海拔高处大于低处,pH值的影响作用并不显著。土壤中无定形铜含量与全铜量的比值,在富铝化程度相类似的土壤上随海拔升高而明显增大,即在红壤、黄红壤和黄壤之间有明显不同。无定形铜含量有随风化淋溶作用增强而降低的趋势。这些可作为土壤分类和肥力评价上的参考。

In the eastern Hebei, North China, the Taipingzbai area is separated from Shuichang area by shear zone. Higher P-T conditions are recorded for Taipingzhai granulites, therefore two areas, representing different crustal levels, were in juxtaposition. The granulite facies orthogneisses from Taipingzhai and the charnockites from Shuichang have strikingly different chemistry. The Taipingzhai granulites are strongly depleted in heat-producing elements and other large ion lithophile elements, whereas, Shuichang charnockites...

In the eastern Hebei, North China, the Taipingzbai area is separated from Shuichang area by shear zone. Higher P-T conditions are recorded for Taipingzhai granulites, therefore two areas, representing different crustal levels, were in juxtaposition. The granulite facies orthogneisses from Taipingzhai and the charnockites from Shuichang have strikingly different chemistry. The Taipingzhai granulites are strongly depleted in heat-producing elements and other large ion lithophile elements, whereas, Shuichang charnockites are enriched in these elements. This is postulated to be due to the action of metamorphic fluids in the lower crust. Different models for source of fluids from both areas have been proposed.

河北东部太古代麻粒岩相深成片麻岩有两种类型:一种亏损放射性生热元素和大离子亲石元素;另一种富集这些元素。该文讨论了这种化学差异及造成差异的原因。

In the fold belt along the north side of the Sino-Korean Platform there occur two ophiolite zones: the Caledonian Ondor Sum ophiolite zone (called the south zone for short) and the early Variscan Solon Mts.-Hegen Mts, ophiolite zone (called the north zone for short).The Ondor Sum ophiolite is the oldest remains of the ancient Mongolian ocean plate subducting by different stages towards the south (towards the continent) and of the Sino-Korean plate accreting towards the north. Thus it is formed by a series of...

In the fold belt along the north side of the Sino-Korean Platform there occur two ophiolite zones: the Caledonian Ondor Sum ophiolite zone (called the south zone for short) and the early Variscan Solon Mts.-Hegen Mts, ophiolite zone (called the north zone for short).The Ondor Sum ophiolite is the oldest remains of the ancient Mongolian ocean plate subducting by different stages towards the south (towards the continent) and of the Sino-Korean plate accreting towards the north. Thus it is formed by a series of tectonic slabs that were obducted southwards in the early part of the Early Paleozoic.From below upwards, the original ophiolite sequence consists of metam-orphic peridotite, harzburgite and bunite ultramaficmafic cumulative complex (including pyroxenite and gabbro), basic lavas with pillow structure and radiolarian siliceous rocks.The north ophiolite zone, extending in a nearly E-W direction, is composed of ophiolites in the Solon Mts, Bumbat, the Hegen Mts., Wusinihei and Meilaotetula, whose age is early Late Paleozoic.The original ophiolite sequence is in ascending order: (1) metamorphic peridotite composed of Iherzolite, harzburgite and dunite (strongly depleted upper mantle); (2) ultramafic-mafic cumulative complex which is composed of dunite, feldspathic dunite and chromite in the lower part, stratified tro-ctolite and gabbro in the middle part, and massive grabbre at the top; and (3) sheeted dike swarms and metamorphic basic lavas.Through studies of the content of general elements,as well as the abundances of trace and rare earth elements, the authors have obtained the following recognitions: (1) In the south zone the metamorphic peridotite is composed of weakly depleted mantle substances; while in the north zone metamorphic peridotite is composed of weakly depleted Iherzolite and strongly depleted harzburgite and dunite. This indicates that the south and north zones are greatly different in the degree of partial melting of the mantle substances. (2) In the ophiolite of the south and north zones there are two suites of basic lavas which are different in age and composition. In the north zone, the metamorphic basic lavas belong to deep-sea tholeiite, characterized by LREE depletion and a low abundance of big-ion elements; while in the south zone, the composition of the basic lavas is near that of slightly alkaline tholeiite, and the lavas are characterized by LREE enrichment and a high abundance of big-ion elements and might be formed in the spreading ridge near the margin of the island arc. (3) During the formation of the Solon Mts. -Hegan Mts. ophiolites, the Xilinhot area at its southern side and the Dong Ujimqin Banner at the northern side respectively belonged to the margins of the south and the north old lands. The chemical characteristics of the volcanic rocks are similar to those of the island-arc lavas, and are greatly different from those of the Hengens Mts. ophiolite. This feature proves that the ophiolite in the north zone not only represents the oceanic crustal fragments of the anciedt Mongolian ocean, but also marks the position of the suture line between the Sino-Korean and Sibrian plates.

中朝陆台北侧褶皱带(中段)中,出露有两条蛇绿岩带:一条是温都尔庙加里东期蛇绿岩带(简称南带);一条是索伦山-贺根山华力西期蛇绿岩带(简称北带)。两条岩带具有不同的时空格局和明显的地球化学差异。通过对两条蛇绿岩带地球化学研究,讨论了蛇绿岩形成的古构造环境。南带蛇绿岩可能是在岛弧边缘附近海盆地扩张脊中形成的;北带蛇绿岩可能是在大洋中脊形成的,它标志着中朝板块和西伯利亚板块之间的碰撞带位置。

 
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