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次生构造
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  secondary structure
     The structure of the adventitious roots induced under the conditions of tissue culture was a typical primary structure and the secondary structure appeared for the first time 68 days after their transplanting.
     在组织培养条件下长出的不定根内部解剖构造为典型的初生构造,移栽后68 d出现次生构造
短句来源
     Results: The results showed that there were secondary structure in the root,and xylem ray were wider than phloem ray.
     结果:光果葶苈的根部有次生构造,木质部射线较韧皮部射线宽广;
短句来源
     From primary structure to secondary structure of the root the number of cortical cells remains the same only their size increases.
     根的皮层细胞从初生构造到次生构造只是体积长大,无数量增加;
短句来源
     Conclusions The secondary structure of the root of Taxus chinensis var. mairei accords with that of other gymnosperms and dicotyledons, although its secondary xylem is constituted with tracheids and sieve cells.
     结论南方红豆杉根的次生构造与其他裸子植物和双子叶植物一致,但次生木质部由管胞,次生韧皮部由筛胞组成。
短句来源
     The results showed that secondary structure of root was undeveloped, there were mass crannies in cortex,vascular bundle were radial pollens were seen, cell wall showed a little thick in common;
     结果表明,金纽扣的显微结构鉴别特征为:根部次生构造不发达,皮层裂隙较多,维管束辐射型,根横切面观细胞壁普遍较厚;
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  “次生构造”译为未确定词的双语例句
     Studies on the Comparison Anatomy of Anomalous Secondary Structure in Rhizoma of Rheum Tanguticum Maxim. Ex Balf. R. Palmatum L. And R. Officinale Baill
     唐古特大黄、掌叶大黄和药用大黄根茎异常次生构造比较解剖学的研究
短句来源
     Study of the Relation Between Antidrought Capability of Trees and Their Secondary Root Structure
     林木抗旱性与其根次生构造关系的研究
短句来源
     The macrostructure of the landform of the North of Guangdong appearsas a net pattern. There are basins in the interiors of nets,mountainous regionsin the arrises of nets.
     粤北地貌宏观结构具网格型式,网格内部是盆地,棱边是山地,属次生构造地貌.
短句来源
     From geological point of view,through the studies of a large quantity of field observations on the relationship between primary/secondary tectonic features of ore/hostrock,hydrothermal substances and mineralisation,the paper provides some evidences to‘synsedimentary theory’.
     本文从地质学角度,通过对碴瓦莫拉矿床矿石和岩石原生构造,次生构造以及热液物质与矿化关系等大量野外观察资料的研究,为“同生沉积说”提供了地质依据。
短句来源
     The root system of ginseng is a tap root system.
     人参(Panax qinseng C. A. Meyer)属于直根系植物,有次生构造
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  相似匹配句对
     “L-STRUCTURE”FOR FUZZY SET IN A LINEAR SPACE
     L—构造
短句来源
     The X.
     在构造 X.
短句来源
     ACTIVE TECTONICS AND ITS SECONDARY DISASTERS ALONG QINGHAI-TIBET LINE
     青藏公路及铁路沿线的活动构造与其次生灾害
短句来源
     SECONDARY STRATOLANDFORM AND NEOTECTONIC DIVISIONS IN THE MOUNTAINS OF HEBEI PROVINCE
     河北山地的次生层状地貌与新构造分区
短句来源
     SECONDARY COLOUR OF JADEITE JADE
     翡翠的次生
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  secondary structure
The secondary structure of catalase was changed by PDSG.
      
Effects of pH, enzyme concentration, and various supplements on the catalytic activity, temperature stability, and secondary structure of horseradish peroxidase (HRP) were studied in diluted aqueous solutions.
      
CaCl2, BSA, and glycerol caused protective effects, whereas KCl, LiCl, maltose, PEG-6000 (at a concentration above 3%), Triton X-100, ethanol, and Kathon CG had an opposite effect and altered the secondary structure of HRP.
      
The secondary structure of its molecule was characterized by a considerable number of α-helices.
      
A study of the secondary structure detected the predominant presence of β-structures, especially antiparallel, in the molecule of this regulatory protein as well as the regions described in terms of a statistical globule.
      
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The structure of the root, stem, rhizome and leaf of Aristolochia mollissima Hance are observed and described in the present paper. Having the epidermis, cortex, starch sheath, perivascular sclerenchyma, six vascular bundles, pith and pith ray, the stem is similar to the root in their structure. In the perenchyma of the secondary structure of stem and root and rhizome and petiole, the secretory cells have been found to disperse. The secretory cells full of yellow essential oil which is just the effective pharmacoutial...

The structure of the root, stem, rhizome and leaf of Aristolochia mollissima Hance are observed and described in the present paper. Having the epidermis, cortex, starch sheath, perivascular sclerenchyma, six vascular bundles, pith and pith ray, the stem is similar to the root in their structure. In the perenchyma of the secondary structure of stem and root and rhizome and petiole, the secretory cells have been found to disperse. The secretory cells full of yellow essential oil which is just the effective pharmacoutial elements. The secretory cells are the largest numbers in the secondary structure of the rhizome and root.

本文观察和描述了绵毛马兜铃的根、茎、根茎及叶的解剖构造。该植物茎与根茎的构造相似,均有表皮、皮层、淀粉鞘、周维纤维、六束维管束、髓及髓射线。笔者发现在其茎、根茎、根和叶柄次生构造的薄壁组织中,存在分散的分泌细胞,以根茎和根中的数量最多。这种分泌细胞所含的黄色芳香油即是药用有效成份之一。

Petrochemical analysis, some trace elements such as Zr Cr, Ti, Sr, and Ni and rare earth element geochemical characteristics have shown that some of volcanic rocks in the ophiolites of later Proterozoic Xuefeng stage are similar to those of mid-oceanic ridges, but others are similar to those of of island arc. In other words, the ophiolites of later Proterozoic Xuefeng stage is an ophiolites complex including two kinds of ophiolites with different origin (ocean-floor origin and island arc origin). It has been...

Petrochemical analysis, some trace elements such as Zr Cr, Ti, Sr, and Ni and rare earth element geochemical characteristics have shown that some of volcanic rocks in the ophiolites of later Proterozoic Xuefeng stage are similar to those of mid-oceanic ridges, but others are similar to those of of island arc. In other words, the ophiolites of later Proterozoic Xuefeng stage is an ophiolites complex including two kinds of ophiolites with different origin (ocean-floor origin and island arc origin). It has been found that some ocean-floor ophiolites contacted with adjoinging rocks by fault, while a few island arc ophiolites contacted with country rocks by intrusion and produced hydrothemal contact metamorphism and minerals. The ophiolites with different emplaced style distributed by paragenesis and non-order in space. It is also confirmd that the ophiolites is an ophiolite complex. The ophiolites complex occurred in the trench-arc system of later Proterozoic Xuefeng stage in the Guiba Longsheng regions and this faot indicates the migration of subduction zone was from northwest to southeast. It consistented with the Southeast China continental crust migration-accretion proposed by Prof. Guo Lingzhi Shi Yangshen et al.

研究表明:蛇绿岩分布于中国东南部江南元古代东安——雪峰期古岛弧褶皱系西端东南缘桂北龙胜一带。呈北东——南西向带状延伸。通过对蛇绿岩常量元素岩石化学特征进行研究,表明龙胜存在代表洋壳碎片的蛇绿岩套与岛弧成因的蛇绿岩组成的一种复合成因蛇绿混杂岩。微量元素(Zr、Cr,Ti、Sr、Ni等)及稀土元素地球化学特征研究同样得到进一步验证。龙胜一带为元古代雪峰期海沟岛弧系。由于大洋板块从龙胜南东大洋一侧向北西运移,并与古扬子大陆板块碰撞俯冲。代表洋壳碎片的蛇绿岩次生构造定位于消减带上,岛弧成因蛇绿岩则由于洋壳物质潜入于上地幔发生部分分熔再生上升侵位形成。龙胜蛇绿混杂岩从北西向南东分布着三门、龙胜二个次一级的楔状蛇绿岩带,即当时至少有过二次板块俯冲增生作用。这一作用从北西向南东逐渐迁移,反映了中国东南部大陆地壳从北西向南东逐渐迁移、增生的演化特征。

Petrochemical analysis, some trace elements such as Zr Cr, Ti, Sr, and Ni and rare earth element geochemical characteristics have shown that some of volcanic rocks in the ophiolites of later Proterozoic Xuefeng stage are similar to those of mid-oceanic ridges, but others are similar to those of of island arc. In other words, the ophiolites of later Proterozoic Xuefeng stage is an ophiolites complex including two kinds of ophiolites with different origin (ocean-floor origin and island arc origin). It has been...

Petrochemical analysis, some trace elements such as Zr Cr, Ti, Sr, and Ni and rare earth element geochemical characteristics have shown that some of volcanic rocks in the ophiolites of later Proterozoic Xuefeng stage are similar to those of mid-oceanic ridges, but others are similar to those of of island arc. In other words, the ophiolites of later Proterozoic Xuefeng stage is an ophiolites complex including two kinds of ophiolites with different origin (ocean-floor origin and island arc origin). It has been found that some ocean-floor ophiolites contacted with adjoinging rocks by fault while a few island arc ophiolites contacted with country rocks by intrusion and produced hydrothemal contact metamorphism and minerals. The ophiolites with different emplaced style distributed by paragenesis and non-order in space. It is also confirmd that the ophiolites is an ophiolite complex. The ophiolites complex occurred in the trench-arc system of later Proterozoic Xuefeng stage in the Guiba Longsheng regions and this faot indicates the migration of subduction zone was from northwest to southeast. It consistented with the Southeast China continental crust migration-accretion proposed by Prof. Guo Lingzhi, Shi Yangshen et al.

研究表明:蛇绿岩分布于中国东南部江南元古代东安——雪峰期古岛弧褶皱系西端东南缘桂北龙胜一带。呈北东——南西向带状延伸。通过对蛇绿岩常量元素岩石化学特征进行研究,表明龙胜存在代表洋壳碎片的蛇绿岩套与岛弧成因的蛇绿岩组成的一种复合成因蛇绿混杂岩。微量元素(Zr、Cr、Ti、Sr、Ni等)及稀土元素地球化学特征研究同样得到进一步验证。龙胜一带为元古代雪峰期海沟岛弧系。由于大洋板块从龙胜南东大洋一侧向北西运移,并与古扬子大陆板块碰撞俯冲。代表洋壳碎片的蛇绿岩次生构造定位于消减带上,岛弧成因蛇绿岩则由于洋壳物质潜入于上地慢发生部分分熔再生上升侵位形成。龙胜蛇绿混杂岩从北西向南东分布着三门、龙胜二个次一级的楔状蛇绿岩带,即当时至少有过二次板块俯冲增生作用。这一作用从北西向南东逐渐迁移,反映了中国东南部大陆地壳从北西向南东逐渐迁移、增生的演化特征。

 
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