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tectonic deformation style
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  构造变形样式
     Based on the structural geometry and kinematics of North Yellow Sea basin,the tectonic deformation style and geodynamic process of North Yellow Sea basin are studied.
     以北黄海盆地构造几何学、运动学特征为基础,探讨了北黄海盆地的构造变形样式及动力学演化过程。
短句来源
  相似匹配句对
     The style of X.
     证书采用X .
短句来源
     Tectonic deformation is complicated and the main tectonic style is compressional reversing fracture.
     它的构造变形十分复杂,盆地构造样式为压性逆冲断裂;
短句来源
     Tectonic style and deformation difference of granite bodies in the opening-closing tectonic setting
     开合构造环境下花岗岩体的构造样式与变形差异
短句来源
     (3) the study of the tectonic deformation of the basin;
     (3)构造变形基本特征研究;
短句来源
     According to the supcrosition of structure clement and deformation style, the Xingdi movement can be divided into three tectonic phase.
     根据构造要素的叠加关系和变形特征,将这次构造运动划分为三个变形幕。
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Tectonic anctivity is strong with a variety of tectonic deformation styles in Zhuanghearea,Liaoning,which reflect,the systematic change of structural deformation from the lowertectonic level to the upper one, and the systematic evolution of progressively decreasing rockductility from the early stage of folding to the late stage of fracturing.The paper outlines thetectonic sequence and analyses the tectonic evolution process by means of structural analyti-cal method.

辽宁庄河地区构造活动强烈,构造变形样式多种多样,反映了在不同体制下,构造变形由下部构造层次到上部构造层次的系统变化,从早期褶皱变形到后则破裂变形过程中岩石韧性递减的系统演变。笔者利用构造解析方法,初步确定了该区的构造序列并探讨了构造演化过程。

Field investigations of the geomorphology of river valleys and neotectonic deformations in the source region of the Yangtze River, northern Tibet, show that the region is characterized by a parallel type drainage pattern and wide and narrow valleys of different shapes. Since the Neogene, the region mainly has undergone a tectonic evolution from compression in the early stage and extension in the late stage, thus forming three tectonic deformation styles, i.e.: folds-thrusts and strike-slip shear...

Field investigations of the geomorphology of river valleys and neotectonic deformations in the source region of the Yangtze River, northern Tibet, show that the region is characterized by a parallel type drainage pattern and wide and narrow valleys of different shapes. Since the Neogene, the region mainly has undergone a tectonic evolution from compression in the early stage and extension in the late stage, thus forming three tectonic deformation styles, i.e.: folds-thrusts and strike-slip shear in the early stage and normal faults and grabens in the late stage. Neotectonic movement has not only controlled the geomorphological features of the river valleys and drainage pattern but also affected the distribution of the river terraces and shape and structure of diluvial (alluvial) fans. The main drainage system in the source region of the Yangtze River formed at least by headward erosion a-long the faults of different natures generated by neotectonic movement during the Holocene.

对藏北长江源地区河谷地貌和新构造变形调查发现,该区具有平行式水系格局,河谷地貌以形态不同的窄谷和宽谷为特点,新近纪以来该区主要经历了早期挤压和晚期伸展构造演化过程,产生了褶皱-逆冲、走滑剪切、正断层和地堑构造3种构造变形样式。长江源区河谷地貌的形成演化明显受新构造运动的影响,新构造运动不仅控制了河谷地貌形态与水系格局,而且影响了河流阶地分布以及洪(冲)积扇的形态、结构。长江源地区主要水系至少自全新世以来是沿新构造运动产生的不同性质断裂构造溯源侵蚀发育而成。

Based on the structural geometry and kinematics of North Yellow Sea basin,the tectonic deformation style and geodynamic process of North Yellow Sea basin are studied.The result shows that there are four kinds of tectonic deformation for North Yellow Sea basin,including extensional structural deformation,compressed structural deformation,shear structural deformation and inverse structural deformation,etc,and the regional geodynamic setting for North Yellow Sea basin were...

Based on the structural geometry and kinematics of North Yellow Sea basin,the tectonic deformation style and geodynamic process of North Yellow Sea basin are studied.The result shows that there are four kinds of tectonic deformation for North Yellow Sea basin,including extensional structural deformation,compressed structural deformation,shear structural deformation and inverse structural deformation,etc,and the regional geodynamic setting for North Yellow Sea basin were mainly the regional extension superimposed by horizontal compressing and correlative shearing,which resulted in extensional faulted basin for North Yellow Sea basin with a series of graben and half-graben mode depressions.The extension,compression,elevation and subsidence of North Yellow Sea basin were controlled by regional extensional and compressional stress field caused by interaction of plates and weak uplifting of asthenosphere underneath,and its geodynamic evolution process included five stages such as extensional fault depression in Late Jurassic-Early Cretaceous,thermo-upwelling in late Cretaceous-Paleocene,rifting in Eocene-Oligocene,structural inversion in late Oligocene-early Neogene and thermo-subsiding in Neogene.

以北黄海盆地构造几何学、运动学特征为基础,探讨了北黄海盆地的构造变形样式及动力学演化过程。研究表明,北黄海盆地的构造变形包括伸展构造变形、挤压构造变形、扭动构造变形以及反转构造变形等,北黄海盆地发育的区域动力学背景即是以区域拉伸作用为主、且叠加有水平挤压作用以及相关的扭动作用,并由此导致了北黄海盆地是以一系列地堑、半地堑式坳陷组成的拉张断陷盆地;北黄海盆地的伸展、挤压与升降作用受控于板块相互作用引起的区域引张与挤压应力场并辅以深部软流圈的微弱上拱隆起作用,其动力学演化过程包括晚侏罗世—早白垩世伸展断陷、晚白垩世—古新世热隆、始新世—渐新世裂陷、渐新世末期—新近纪早期构造反转以及新近纪热沉降等5个阶段。

 
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