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构造分层
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  tectonic layering
     Likewise, the tectonic layering of the crust was clearly revealed, which should be an important basis, significantly, for the characteristic analysis and an information for establishing digital base of the geology and geophysics of the shallow level in the Upper Yangtze plate tectonics.
     同时,也揭示了地壳的构造分层性,并可作为上扬子板块浅层地质—地球物理特征分析的重要依据和建库信息。
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  “构造分层”译为未确定词的双语例句
     ON THE TECTONOLAYERING, RHEOLOGICOLAYERING AND CHEMICOLAYERING TAKING DIPSLIP FAULT SYSTEMS OF THE MIDDLE LOWER YANGTZE AREA AS AN EXAMPLE
     论构造分层、流变分层和化学分层作用——以中下扬子区倾滑断裂系统为例
短句来源
     MULTI-LEVEL STRONGLY CONSTRUCTIVE LEARNING ALGORITHM OF RECURSIVE LOGIC PROGRAM AND ITS REALIZING
     递归逻辑程序的强构造分层学习算法及其实现
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     Combining three parameters, which include the number of heating lines, the space between lines and the shrink quantity of line, HGA coding is constructed, and then three parameters of automatic processing for line heating, such as processing speed, length of heating line and shrinkage of heating line, are gained.
     由加热线条数、相邻加热线之间距离(加热线间距)和加热线收缩量3个参数构造分层遗传算法编码,最终得到加工速度、加热线长度和加热线位置3个水火弯板自动化加工参数,在此基础上,应用Visual C++6.0软件设计开发了“水火弯板自动化加工工艺参数优化系统”。
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     The differential layering or metamorphic layering of these faults (among 1S、4S detachment beds to be stressed) were discussed with the quantitative parameters of the tectonolayering, rheologicolayering and chemicolayering.
     并以构造分层、流变分层和化学分层系统定量参数论述这些断裂(侧重其中1S、4S滑脱层)中的分异分层或称变质分层作用。
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     By this way, the additional displacement fields satisfying the displacement boundary conditions of the delamination area can be established.
     通过切取纵横切片,利用含分层层合直梁与曲梁的附加位移,构造分层区附加位移模态。
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  相似匹配句对
     STRATIFYING METHOD FOR CONSTRUCTING ORTHOGONAL ARRAYS
     构造正交表的分层方法
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     “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
     4. stratification and zonation of tectonics.
     (4)构造类型的分布具有分层分带性。
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     social stratification
     社会分层
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  tectonic layering
Study of tectonic layering motion and layering mineralization in the Tongling metallogenic cluster
      
Analysis of the deep tectonics and cover tectonic deformations shows that tectonic layering motion is a typical lithospheric characteristic in the Tongling area and the metallogenic belt of the middle-lower Yangtze.
      
Controlling of the deep tectonosphere over the shallow-seated tectonosphere involves various grades of tectonic layering motions.
      
Multi-layer, multi-grade, and multi-directional gliding tectonics are the specific modes of tectonic layering motions in the cover of the Tongling metallogenic cluster.
      
Under these conditions the lithosphere heterogeneities (composi tion, rheological) create the prerequisites for the development of various phenomena of tectonic layering (lateral shearing, different deformation of layers).
      
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In order to reveal the texture characteristic of the crust and a relationship between the structure and mineralization in the Middle Lower Yangtze area, samples overall selected of the rock mechanics、rock rheology and rock chemistry have been determined and analysed in the studied area; six suits of regional oriented layerslip dipslip fault systems were subdivided up. The differential layering or metamorphic layering of these faults (among 1S、4S detachment beds to be stressed) were discussed with the quantitative...

In order to reveal the texture characteristic of the crust and a relationship between the structure and mineralization in the Middle Lower Yangtze area, samples overall selected of the rock mechanics、rock rheology and rock chemistry have been determined and analysed in the studied area; six suits of regional oriented layerslip dipslip fault systems were subdivided up. The differential layering or metamorphic layering of these faults (among 1S、4S detachment beds to be stressed) were discussed with the quantitative parameters of the tectonolayering, rheologicolayering and chemicolayering. In general, the rheological layering is regarded as a principal part of the metamorphic layering, and the tectonic layering is taken for a foundation. Obviously the chemical layering is as deepening research and succeeding interpretation. Otherwise in this area under these layering actions controllign the differential textures within orders and bands more tend towards consummation in the stratabound ore deposits concerning the dynamic forming rock and ore system (4S、5S and 6S as the represenative), and they are on the coincidence relations between strata, faults and beds.

为揭示中下扬子区地壳结构特征和构造与成矿的相关性,在区内全面探集岩石力学、岩石流变和岩石化学样品测试分析,划分出六套层滑一倾滑区域性导位断裂系统。并以构造分层、流变分层和化学分层系统定量参数论述这些断裂(侧重其中1S、4S滑脱层)中的分异分层或称变质分层作用。通常以流变分层作为变质分层研究的主体,构造分层为基础,化学分层则是研究的深入和继续。区内在这些分层作用制约下所形成的动力成岩成矿层控矿床中(4S、5S和6S尤为典型),层次层带分异结构更趋完善,地层—断层—矿层三位统于一体

In this paper we introduced a strongly constructive multi-level learning algorithm, and used it to solve a type of strongly constructive two-level learning problem。It will provide a new way for further research on strongly consctructive learning ,and discused the relative problems in detail.

本文提出了一种逻辑程序的强构造分层学习算法 ,用该算法解决了一类递归逻辑程序的强构造二层学习问题 ,为强构造学习研究提供了一个新的思路 ,并就有关问题进行了详细的讨论

The thin skinned layer block structures confined by the reverse dip slip fault in a leading edge,normal dip slip fault in a back edge and strike slip faults (lateral sinistral and/or dextral fault)widely developed in the middle lower Yangtze River area,may result from layering of rock materials and energy,and structures as well as layer sliding. The mechanism for the dip slip and strike slip in the layer block structure in the shallow crust is similar to that in terrane and plate tectonics at depth,and...

The thin skinned layer block structures confined by the reverse dip slip fault in a leading edge,normal dip slip fault in a back edge and strike slip faults (lateral sinistral and/or dextral fault)widely developed in the middle lower Yangtze River area,may result from layering of rock materials and energy,and structures as well as layer sliding. The mechanism for the dip slip and strike slip in the layer block structure in the shallow crust is similar to that in terrane and plate tectonics at depth,and to the origin of the slip apart and tear apart fractures in fracture mechanics and the knifeedge and helical dislocations in solid physics.

中、下扬子区广为发育的前缘逆向倾滑,后缘正向倾滑和两侧为走滑断裂所限的薄皮层块构造,系挤压和拉张作用处于同一运动系统中,是由岩石的物质分层、能量分层和构造分层作用及层滑运动所致。地壳表、浅层分布的层块构造与深层的块片构造、地体构造和板块构造的倾滑、走滑机制是一致的,并与断裂力学中的滑开型、撕开型和位错构造中的刃型位错、螺型位错的力学机理和运动本质是相同的

 
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