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Anticlines and synclines are the basic deformation forms of sedimentary basins,as well as neutral plane s are the important interface of strata deformation.
背斜、向斜褶皱构造是沉积盆地的基本形变,中和面也是地层变形中的重要界面,在传统的石油地质理论中,一直忽视了这一重要界面。
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Anticlines and synclines are the basic deformation forms of sedimentary basins, as well as neutral planes are the important interface of strata deformation. But the neutral plane is paid no attention in the traditional petroleum geological theory.
背斜、向斜褶皱构造是沉积盆地的基本形变,中和面也是地层变形中的重要界面,在传统的石油地质理论中,一直忽视了这一重要界面。
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That is structural highs in overburden of salt are corresponding to the synclines in subsalt layers and anticlinal flanks of overburden are corresponding to anticlinal highs in subsalt layers.
即盐上层构造高点对应盐下层向斜和盐上层背斜翼部对应盐下层背斜高点。
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The main fold in the mining area is a compound syncline, composed of two sub synclines and one sub anticline.
矿区主干褶皱为一复式向斜,由2个次级向斜和1个次级背斜组成。
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According to their forms and the stratigraphic facing, folds can be subdivided into anticlines and synclines.
P13 根据褶皱的形态和组成褶皱的地层面向,将褶皱进一步分为两种基本类型:背斜和向斜。
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