tectonic

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造性移动。

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

洞庭湖是由造动奠定基本格局，又叠加了用以及人类活动多因素混成湖。

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

腾冲火山区造应力场主要为北北东—北东—北东东向，接近水平压应力场。

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

形成异常地层压力原因主要有成岩用、热力用、生化用、造用、渗析及流体密度差异用等。

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

该盆地层序划分及动力学分析对黑龙东部白圣纪地层对比、造用及成矿用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.

金矿形成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.

区域造应力场对于研究地震成因、地震预报和地球动力学都具有重要意义。

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

滑脱断裂造样式，以短轴背形、向形造为主，另有穹窿造、滑来峰造、滑覆窗造。

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原始造格局和沉积特征，就必须除去后期叠加造层和造变形，即反序造分析法。

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.

通过造地貌和造年代学分析方法，对其表现特徵和动特徵及其与铀成矿之间关系进行研究。

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《中国主要地质造单位》中,他用阿尔冈活动论思想,阐述了中国大地造动力演化过程。

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