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tectonic layering
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  构造分层
     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。
短句来源
  “tectonic layering”译为未确定词的双语例句
     Geologists of the former Soviet Union describe it as tectonic layering of the lithosphere.
     前苏联地质学家把它称为岩石圈的构造成层作用。
短句来源
  相似匹配句对
     Tectonic in Architecture
     论建筑中的结构造型
短句来源
     and tectonic movement.
     (3)与深部地质作用有关;
短句来源
     Geologists of the former Soviet Union describe it as tectonic layering of the lithosphere.
     前苏联地质学家把它称为岩石圈的构造成层作用。
短句来源
     Network Layering and Segmentation
     网络的分层和分割
短句来源
     THE LAYERING OF DEEP KARST IN VALLEYS
     河谷深岩溶的成层性——以辽宁观音阁水库为例
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  tectonic layering
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).
      
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.
      
Controlling of the deep tectonosphere over the shallow-seated tectonosphere involves various grades of tectonic layering motions.
      
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.
      
Study of tectonic layering motion and layering mineralization in the Tongling metallogenic cluster
      
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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

Diffusive deformation of the interior of the continental lithosphere indicates that the continental tectonics is different from plate tectonics. Laboratory measurements of mineral deformation, change in rheological behavior of rocks with depth and seismic sounding data all show jelly sandwich-like strength envelopes of the continental lithosphere. Ren Ji-shun, Zhang Guo-wei and Zhong Da-lai call these 3-D crossing structures at different levels of the lithosphere as the overpass architecture or multi-oriented...

Diffusive deformation of the interior of the continental lithosphere indicates that the continental tectonics is different from plate tectonics. Laboratory measurements of mineral deformation, change in rheological behavior of rocks with depth and seismic sounding data all show jelly sandwich-like strength envelopes of the continental lithosphere. Ren Ji-shun, Zhang Guo-wei and Zhong Da-lai call these 3-D crossing structures at different levels of the lithosphere as the overpass architecture or multi-oriented layered structure separately. Its occurrence implies the tectonic decoupling in the lithosphere, and the new tectonic regime evolving on the detachment surface. Geologists of the former Soviet Union describe it as tectonic layering of the lithosphere. In the paper the authors cite some examples of overpass architectures possibly exposed in eastern and western syntaxes of the Himalayan orogen and the southern Qinling orogen and appear for geologists to pay attention to it and take it as a best penetrating point to approach the deformation of the continental lithosphere.

大陆内部弥散性的变形表明经典板块构造理论未能阐述大陆构造。矿物变形的实验室研究结果、岩石流变学性质随深度改变和地震测深剖面资料都提示大陆岩石圈具有三明治式的强度包络面。任纪舜、张国伟和钟大赉分别把岩石圈不同深度层次的三维交切构造称为立交桥式构造或多向层架构造。它们的出现提示岩石圈发生了构造解耦,新的变形体制在拆离面以上发展起来。前苏联地质学家把它称为岩石圈的构造成层作用。本文列举了喜马拉雅东、西构造结和秦岭造山带可能出露于地表的三维交切构造实例,呼吁重视这类代表大陆岩石圈不同深度层次的构造堆叠体,并把它作为揭示岩石圈构造变形的最佳切入点。

Based on a study of physico-mechanic parameters of rocks to regional slipping layers in the Middle-Lower Yangtze crust, the relative parameters of rock physico-mechanics to regional slipping layers were systematically and quantitatively determined in the Upper Yangtze crust. The slipping layers indicated a characteristic regularity in the plasticity, ductility and viscosity, which possessed a number of universality and contrast in the digital strata of the southern pattern in China. Likewise, the tectonic...

Based on a study of physico-mechanic parameters of rocks to regional slipping layers in the Middle-Lower Yangtze crust, the relative parameters of rock physico-mechanics to regional slipping layers were systematically and quantitatively determined in the Upper Yangtze crust. The slipping layers indicated a characteristic regularity in the plasticity, ductility and viscosity, which possessed a number of universality and contrast in the digital strata of the southern pattern in China. 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.

在中下扬子地区地壳区域性滑动层位岩石物性力学参数研究的基础上,对上扬子地区地壳的相应岩层进行了系统的定量测试。其滑动层位各种参量在塑性、韧性和粘性上所表现出特征的规律,在我国南方型数字地层中,具有一定的普遍性和可比性。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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