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tectonic modeling
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  构造建模
     Research of Tectonic Modeling and Petroleum Accumulation Elements for South Margin of Junggar Basin
     准噶尔盆地南缘构造建模及油气成藏条件研究
短句来源
     TECTONIC MODELING AND SEISMIC DATA TECTONIC INTERPRETATION IN EAST MICHANGSHAN AND WEST DABASHAN FRONT,SICHUAN BASIN
     四川盆地米仓山东端—大巴山西段前缘构造建模及地震资料构造解释
短句来源
     By using the theory of fault-related fold and kinematics characters, research of tectonic modeling about local structures of south margin of Junggar basin was made.
     利用断层相关褶皱理论、运动学特征,对准噶尔盆地南缘区域局部构造进行了构造建模研究。
短句来源
  构造模拟
     The most important one of them is tectonic analysis method, whose key factors are to remove deformation and structural layer. The author thinks that the key technologies for analyzing relict basins are tectonic imagining, tectonic ageing and tectonic modeling.
     认为去变形和去构造层是残余盆地构造分析的两个关键环节 ,而构造成像技术、构造测年技术和构造模拟分析技术是残余盆地构造分析的关键技术 .
短句来源
     The methods of paleomagnetism,magnetic fabric,tectonic analysis,high-accuracy GPS monitoring and tectonic modeling can be used to identify these rotations,but the combination of the methods are very important to get a reliable result.
     运用古地磁学、磁组构、构造分析、高精度GPS监测及构造模拟等方法,可以对这些构造及块体的旋转方向和幅度进行研究。
短句来源
  “tectonic modeling”译为未确定词的双语例句
     LITHOSPHERIC CHARACTERISTICS AND EFFECTIVE ELASTIC THICKNESS OF WESTERN ZENGMU BASIN, SOUTH CHINA SEA: CONSTRAINTS FROM TECTONIC MODELING
     曾母盆地西部岩石圈特性与有效弹性厚度:来自构造模拟的约束
短句来源
     An Asymptotic and Tectonic Modeling Method by Formative RLC Cells for Lossy Transmission Lines
     一种基于RLC元包的有损传输线的渐近式构造模型
短句来源
     Kinematic rheological models are adept in tectonic modeling, but identical with kinematic models in heat flow prediction;
     运动学—流变学模型的优势在于构造演化模拟 ,在热演化方面类似于运动学模型 ;
短句来源
  相似匹配句对
     TECTONIC-THERMAL MODELING OF RIFTING BASIN
     裂陷盆地构造-热演化模拟
短句来源
     Modeling and Application
     化归以及应用
短句来源
     Modeling and Identification
     建模与辨识
短句来源
     and tectonic movement.
     (3)与深部地质作用有关;
短句来源
     Criticize and Tectonic
     批判与建构
短句来源
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  tectonic modeling
Mantle Convection Modeling with Viscoelastic/Brittle Lithosphere: Numerical Methodology and Plate Tectonic Modeling
      


Tectono thermal modeling is based on the geological geophysical models of basin formation, which include kinematic model, kinematic rheological model and dynamic model. Kinematic models have predominance in predicting heat flow but weakness in simulating basin geometry; Kinematic rheological models are adept in tectonic modeling, but identical with kinematic models in heat flow prediction; Dynamic models contain latent advantages and also some obstacles in tectono thermal modeling. Future study...

Tectono thermal modeling is based on the geological geophysical models of basin formation, which include kinematic model, kinematic rheological model and dynamic model. Kinematic models have predominance in predicting heat flow but weakness in simulating basin geometry; Kinematic rheological models are adept in tectonic modeling, but identical with kinematic models in heat flow prediction; Dynamic models contain latent advantages and also some obstacles in tectono thermal modeling. Future study should put emphasis on further improvement of tectono thermal models and its matching with reverse models.

沉积盆地构造热演化模拟建立在盆地成因的地质地球物理模型基础之上 ,其中包括运动学模型、运动学—流变学模型和动力学模型。运动学模型在预测盆地热流演化方面具有优势 ,但在预测构造沉降等几何形态方面存在一定的缺陷 ;运动学—流变学模型的优势在于构造演化模拟 ,在热演化方面类似于运动学模型 ;动力学模型蕴含着潜在的巨大优势 ,只是目前还存在一些阻碍因素。构造热演化正演模型的进一步完善及正、反演模型的匹配将是未来构造热演化模拟的发展趋势

Based on previous researches, evolution mechanism and distribution characteristics of relict basins are stated. The methods of studying relict basins are listed. The most important one of them is tectonic analysis method, whose key factors are to remove deformation and structural layer. The author thinks that the key technologies for analyzing relict basins are tectonic imagining, tectonic ageing and tectonic modeling. The research result in the paper indicates that Shiwandashan Basin is a marine facies...

Based on previous researches, evolution mechanism and distribution characteristics of relict basins are stated. The methods of studying relict basins are listed. The most important one of them is tectonic analysis method, whose key factors are to remove deformation and structural layer. The author thinks that the key technologies for analyzing relict basins are tectonic imagining, tectonic ageing and tectonic modeling. The research result in the paper indicates that Shiwandashan Basin is a marine facies relict basin, and that it is the result of the collision of ancient Western Pacific Ocean Plate, Indosinian Plate and Huanan Plate.

在回顾残余盆地研究现状的基础上 ,从解剖残余盆地成因机制及其分布特征入手 ,详细阐述了残余盆地的研究思路及方法 ,提出研究残余盆地应以构造分析为主线进行 .认为去变形和去构造层是残余盆地构造分析的两个关键环节 ,而构造成像技术、构造测年技术和构造模拟分析技术是残余盆地构造分析的关键技术 .研究结果表明 :十万大山盆地是在古西太平洋板块、印支板块与华南板块三者碰撞拼合作用的基础上发育而成的一个海相残余盆地

The rotations is produced not only by the large movement of the main strike-slip fault,but also by the horizontal movement of the secondary faults within the main fault or in the adjacent area.Although some dynamic models have been proposed to illustrate the relationship between vertical axis rotations and fault slips,it is very difficult to find a simple model to explain the mechanism of the rotations and strike-slip fault systems because of the difference of the deformation environment and boundary conditions...

The rotations is produced not only by the large movement of the main strike-slip fault,but also by the horizontal movement of the secondary faults within the main fault or in the adjacent area.Although some dynamic models have been proposed to illustrate the relationship between vertical axis rotations and fault slips,it is very difficult to find a simple model to explain the mechanism of the rotations and strike-slip fault systems because of the difference of the deformation environment and boundary conditions in different strike-slip fault systems.In many strike-slip tectonic settings,rotations of faults and blocks have been inferred from both laboratory modeling and field geological surveys.Studies show that tectonic rotations related strike-slip faults are very distinct in the areas such as the western coast near the San Andreas fault,the Lake Mead fault in the Basin and Range Province in the United States,the Ailaoshan-Red River fault in Southeast China,the Alpine fault in New Zealand and the Northern Anatolian fault in Turkey.The methods of paleomagnetism,magnetic fabric,tectonic analysis,high-accuracy GPS monitoring and tectonic modeling can be used to identify these rotations,but the combination of the methods are very important to get a reliable result.Much attention should be paid to the tectonic regime and geography changes resulted from tectonic and block rotations during the study of the strike-slip faults,especially the large-scale strike-slip fault systems.

与大型走滑断裂有关的旋转一方面起因于断裂带的大规模走滑,另一方面也与大断裂带内部及外围次级断裂系的水平运动密切相关。尽管前人提出了一些有关断裂带走滑与旋转的动力学模式,但由于不同走滑断裂系变形环境及边界条件的差异,断裂走滑导致块体旋转的机制是非常复杂的,很难用统一的动力学模式来解释。对美国西海岸圣安德列斯断裂、美国盆岭区LakeMead断裂系、中国西南哀牢山-红河走滑断裂系以及新西兰Alpine断裂带、土耳其北安那托利亚断裂等的研究结果均表明,在断裂带走滑过程中,相关构造及块体的旋转非常明显。运用古地磁学、磁组构、构造分析、高精度GPS监测及构造模拟等方法,可以对这些构造及块体的旋转方向和幅度进行研究。由于大规模旋转会导致构造格局及地质地貌特征的改变,因此在走滑断裂带的研究中必须加以重视。

 
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