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style and property
相关语句
  风格性能
     Style and Property of Liquid Ammonia Finished Fabric
     液氨整理织物风格性能研究
短句来源
  “style and property”译为未确定词的双语例句
     Style and Property of Modal Fiber Fabric
     Modal纤维织物风格与性能
短句来源
     During the neotectonie period, there existed differences in different sections of the Sihui-Wuchuang fault zone in intensity, style, and property of tectonic activity, showing a sectional differentia in space.
     在新构造时期、该断裂带不同地段构造活动的强度、方式、性质均有差异,表现出空间上的分段性。
短句来源
     Style and property of fine count high density statin drill fabric, parameter and effect of size matching technology & sizing and weaving technology in production are introduced.
     介绍了细号高密贡缎织物的织物风格和特点,生产过程中的浆纱配浆工艺、浆纱工艺及织造工艺的参数设置和织造效果。
短句来源
     This paper summarizes and analyses the style and property of purifier for indoor air in market. It points out the several critical problems restricting nano- TiO2 purifier applying in industry and domestic. PIP natural accelerant and effect of degradation under the condition of natural light irradiating are introduced in this paper.
     文章概括分析了了现有市场上的空气净化器的分类及特点,及目前制约纳米TiO2空气净化器应用的几个突出问题,并且介绍了新型的PIP自然触媒净化材料和此种材料在自然光照射条件下的降解VOCs 的效果.
  相似匹配句对
     The style of X.
     证书采用X .
短句来源
     property;
     性质;
短句来源
     Style and Property of Modal Fiber Fabric
     Modal纤维织物风格与性能
短句来源
     Style Is an Important Property of Subject
     作风是主体的一个重要规定——论作风的内涵、特征及建设
短句来源
     Style and Property of Liquid Ammonia Finished Fabric
     液氨整理织物风格性能研究
短句来源
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Based on gravity and magnetic data the existance and boundary of palaeo-Junggar land were discussed.The continental shallow-sea deposits of Palaeozoic were believed to overly the Junggar land. The frontland depression and sedimentary characteristics suggest that the Junggar basin was formed during the C2-P1,and its primary boundary line was discussed. The structural evolution of the basin includes four stages. The development of depression and uplipt is zhown in succession. The structural style and property,and...

Based on gravity and magnetic data the existance and boundary of palaeo-Junggar land were discussed.The continental shallow-sea deposits of Palaeozoic were believed to overly the Junggar land. The frontland depression and sedimentary characteristics suggest that the Junggar basin was formed during the C2-P1,and its primary boundary line was discussed. The structural evolution of the basin includes four stages. The development of depression and uplipt is zhown in succession. The structural style and property,and the margin are dominated by nappe structure,and the central part dominated by overlap structure. The principal of structural division was drawn and the structural division was done. The oil source is mainly of P2,follwed by P1,J3and J1+2. Coupled with thermal evolution the oil source abundance index was established, especially the deepseated depression of multiphasal overlapping at the southern margin is the highest in terms of oil source abundance. There are many sets of oil reserviors. P2-J is the main compound oil bearing association. Coupled with the structural development,the oil-gas migration direction was analyzed. Four favourable oil-gas bearing zones were pointed out,that is,Kewu fault steps-Mahu anticline zone,Zhongguai convex-Hongche fault steps. Baijiahai cenves, Mosuowan anticline belt-Shinan convex. The regional exploration should be strengthened. The search of big oil field should start from big depression. The exploration of the Permian and Jurassic should be done contempareously. The selection of the target area should consider the concentration condition of oil and gas at first,then the depth of target formations and drilling condition.

依据重磁力和地壳厚度等资料,论述了准噶尔古陆片的存在及其边界,并认为其上有古生代的陆表海沉积。依据山前凹陷的存在及沉积特征,认为盆地形成于中石炭—早二叠世,并讨论了盆地的初始边界,把盆地形成后的构造演化阶段划分为4个:坳陷和隆起的发育具有继承性特征;构造的样式和性质,边缘以推覆构造为主,中部以披覆构造为主;拟定了构造分区原则,对盆地进行了构造分区。生油层主要是上二叠统,其次是下二叠统、上三叠统和下中侏罗统。结合热演化史,建立了油源丰度指数指标,坳陷特别是南缘多期叠合的深坳陷,是油源丰度最高区。储集层是多套的,上二叠统一侏罗系是最主要的复式含油组合。结合构造发展,分析了油气运移方向,指出了最有利的含油气区带有4个:克乌断阶带—玛湖背斜区,中拐凸起—红车断阶带,白家海凸起,莫索湾背斜带—石南凸起。在勘探方向上,仍应加强区域勘探,立足大坳陷寻找大油田,选区首先考虑油气聚集条件,其次才是目的层深度和钻探条件等。

Unconsolidated Quaternary sediments are widely distributed on the Earth surface. As active faults usually disturb the Quaternary sediments, the study of the deformation styles of these sediments is therefore of great significance to the assessment of fault activity and property. Oriented samples of unconsolidated Quaternary sediments deformed by faulting have been collected from some typical active fault profiles. They were solidified in lab by filling epoxy resin diluted by acetone with solidified agent....

Unconsolidated Quaternary sediments are widely distributed on the Earth surface. As active faults usually disturb the Quaternary sediments, the study of the deformation styles of these sediments is therefore of great significance to the assessment of fault activity and property. Oriented samples of unconsolidated Quaternary sediments deformed by faulting have been collected from some typical active fault profiles. They were solidified in lab by filling epoxy resin diluted by acetone with solidified agent. Oriented thin sections were cut according to the primitive orientations of the samples in the field. Deformation features of the samples were observed carefully under optical microscope. An attempt has been made to identify the deformation microstructures of the samples, which may reflect the features of faulting. The observations show that the deformation in unconsolidated Quaternary sediments can be classified into two styles: fracturing and flow. The fracturing deformation is represented by parallel slip bands, straight slip planes, broken mineral grains etc, while the flow deformation is characterized by flow structures, mineral grain rotation, drag structure of clay minerals and others. The deformation style and property of unconsolidated Quaternary sediments depend to a large extent on the characteristics of the sediments themselves. Unconsolidated Quaternary sediments are composed mainly of clastic grains and clays. They can be considered as a visco-elastic body, and may behave as elastic-plastic materials. The duration of applied force has a great effect on the deformation behavior of unconsolidated Quaternary sediments. It means that strain rate plays an important role in the deformation behavior of unconsolidated Quaternary sediments. It is suggested that the fracturing deformation is generated by high strain rate event such as earthquake, while the flow deformation is generated by low strain rate event such as creep slip. The detailed observation of deformation styles of unconsolidated Quaternary sediments,therefore, may provide important information on the kinetic process of faulting.

选择了一些典型活断层地质剖面 ,对经受了构造变动的第四纪松散沉积物进行了定向原状样品采集。通过室内样品固结、显微薄片制作和显微构造现象观察 ,从显微域里找到了第四纪松散沉积物变形的一些特点 ,并进行了分类。第四纪松散沉积物的变形类型有两种 :一种是破裂变形 ,主要表现为平行滑动条带、平直滑动界面、碎屑颗粒的破碎等 ;另一种是流动变形 ,主要表现为 :流动构造、碎砾旋转、粘土矿物的拖曳滑动等。

Using the properties of high-shrinkage polyester yarn shrinked by thermo-hydro processing, Double-faced water crape fabric and interchangable double-weave fabric are developed. This paper introduces their process technology,analyzed the fabric style and property.

利用高收缩涤纶丝热湿处理产生收缩的特性 ,开发了双面水纹绉和表里换层高花织物 ,对织物的生产工艺作了介绍 ,分析了织物的风格特点及性能

 
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