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1)  side component
板侧构造
1.
It analyzes the reasons of floor board vertical cracks,from emphasizing and raising cracks quality,choosing rational board side component forms,cleaning board surface,strengthening floor component quality management,brings forward the protecting measures of vertical cracks,in order to ensure the normal and safe use of floor surface.
详细分析了楼地面沿板缝方向产生纵向裂缝的原因,从重视和提高嵌缝质量、选择合理的板侧构造形式、清洗板面、加强楼板构件的质量管理等方面提出了纵向裂缝的防治措施,以保证楼地面的正常安全使用。
2)  lateral desplacement resistant construction
抗侧移构造
3)  plate tectonics
板块构造
1.
Control of plate tectonics over evolution of petroliferous basins and characteristic of oil and gas distribution in China;
中国板块构造对油气盆地演化和油气分布特征的控制
2.
Charm of landing of plate tectonics on the continent as viewed from the study of the archipelagic arc-basin system;
从多岛弧盆系研究实践看板块构造登陆的魅力
3.
Present-day mantle flow and its interaction with plate tectonics inferred from observational evidence;
现今的地幔流动及其与板块构造的相互作用:从观测证据得到的推论
4)  plate structure
板块构造
5)  Plate tectonic
板块构造
1.
In recent years, many Proterozoic ophiolites are identified,which indicate that modern plate tectonics could be extrapolated at least to the Early Proterozoic, and Wilson cycle has been operated since then.
太古宙科马提岩—拉斑玄武岩普遍与地幔柱的热点活动有关,地幔柱在早太古代构造演化过程中起重要作用,是板块构造的重要补充机制。
2.
Since the advent of plate tectonics, mountain-building is generally referred toas a result of collision between oceanic plate and continental plate or continentalplate and continental plate.
本文根据对中国重要蛇绿岩带的观察,并参考大量国内外文献,对板块构造学说的造山模式提出了否定意见,认为古老山系和现代山系的形成都与板块构造碰撞无关,并提出大陆内部山系形成与盆地形成研究的必要性。
3.
To divide plate tectonic units,as the author held,the four basic principles should be fol-lowed,that is,systematic principle,space-time principle,grade-order principleand synthetic principle.
作者认为板块构造单元划分应遵循4个基本原则,即系统原则、时空原则、层次原则,综合原则。
6)  intraplate tectonics
板内构造
1.
In terms of the characteristic of interior tectonic deformation in the Yangtze plate and the stage of development and evolution in geohistory, its formed mechanism of the intraplate tectonics is treated in this paper, and the conclusion that the downgoing pattern within the lithosphere can be applied to account for its thin-skin tectonic is made out.
本文在概略分析扬子板块内部构造变形特征和地史发展演化阶段的基础上 ,初步探讨了该板内构造形成的机制 ,认为其薄皮构造可用“岩石圈内俯冲作用模式”予以解释。
补充资料:侧侧
1.多貌。 2.寒貌。 3.象声词。叹息声。 4.指其他声音。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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