This crisis possibly causes the world civilized tectonic plate's constructivity migration.

这场危机可能导致世界文明板块的性移动。

Dongting basin was shaped not only by tectonic movement but also by potamic and anthropogenic influence.

洞庭湖是由动奠定基本格局，又叠加了江河作以人类活动的多因素的混湖。

The tectonic stress field in Tengchong volcano areas is oriented as NNE-NE-NEE, nearing horizontal compr essive stress field.

腾冲火山区应力场主要为北北东—北东—北东东向，接近水平的压应力场。

The reasons forming abnormal formation pressure mainly includes digenesis, thermogenesis, biochemical action, tectonic action, dialysis, and fluid density difference action.

形异常地层压力的原因主要有岩作、热力作、生化作、作、渗析流体密度差异作等。

The sequence classification and dynamic analysis of this basin provide an important evidence to the stratigraphic correlation, tectonic analysis and minerogenesis.

该盆地的层序划分动力学分析对黑龙江东部白圣纪地层对比、作矿作的分析提供了重要依据。

Characteristics of plastic deformation of stress minerals in veins, such as subgrain tectonics, deformation, lamellae and deformation bands, can be found.

金矿的形富集与韧性剪切带多期(次)活动密切相关，尤其是韧脆性变形期。

As is well known the regional tectonic stress field is of great importance to the study of seismogenesis, earthquake prediction and earth dynamics.

区域应力场对于研究地震因、地震预报和地球动力学都具有重要的意义。

The styles of the detachment structure are short antiform and synform structure mainly, and dome structure, nappe outlier and nappe tectonic window too.

滑脱断裂的样式，以短轴背形、向形为主，另有穹窿、滑来峰、滑覆窗。

Then use antitone structural analysis method to recognize and reconstruct the primary tectonic structure and sedimentary feature of a basin in certain geological history.

要认识和重建某个地质历史时期盆地的原始格局和沉积特征，就必须除去后期叠加的层和变形，即反序分析法。

By using the approach of morphostructure and tectonic chronology analysis, neotectonic activity evidences and characteristics as well as its ralation to uranium mineralization were researched.

通过地貌和年代学的分析方法，对其表现特徵和动特徵其与铀矿之间的关系进行研究。

Argand's mobilism thought as to the dynamical evolution process of the tectonics in On Major Tectonic Forms of China. Then, he absorbed the quintessence of A.

在《中国主要地质单位》中,他阿尔冈活动论的思想,阐述了中国大地的动力演化过程。

The basin tectonic model: it is intermont basin during late Jurassic to early Cretaceous, developed into faulted-lacustrine basin in Eogene, and evolved into depression in Neogene and Quaternary.

“盆地”发育模式为：从晚侏罗世到白垩纪末期发育的山间“盆地”开始、发展到早第三纪断陷湖盆的发育、再演化为晚第三纪第四纪地陷发育阶段。