The stratigraphic order, feature, sedimentary environment, original tectonic environment of Pre-Nanhua system are discussed on the basis of division of stratigraphic tectonic area.
在地层构造区划分的基础上，系统论述了前南华纪岩石地层层序、宏观特征、沉积环境、原始构造环境。
The 5 first order tectonic sequences show that the 5 types of basins are formed in 5 evolution stages.
一级构造层序揭示了盆地经历了5个构造演化阶段，形成5个盆地原型。
It is significant to know changing character of lithosphere structure in order to analyze and study regional tectonic conditions, stress field and earthquake occurrence.
了解和认识岩石圈结构及其变化特征，对于分析研究该区域构造环境、应力场和地震的发生等有重要意义。
The stress action of second order tectonic stress district shows coherence in a relatively large area. This stress field is controlled by regional block interaction.
二级构造应力区受控于区域块体间的相互作用，在较大区域范围内应力作用具有较强的相关性；
Long-term surface denudation rates are in first order controlled by tectonic uplift and could reflect the geomorphical evolution under the influence of tectonics.
长尺度地表剥蚀速率在根本上受控于构造作用，并且能够反映构造影响下的地貌发育过程。
The stress action of second order tectonic stress district shows coherence in a relatively large area.
二级构造应力区受控于区域块体间的相互作用，在较大区域范围内应力作用具有较强的相关性；
The stress action of second order tectonic stress district shows coherence in a relatively large area.
二级构造应力区受控于区域块体间的相互作用，在较大区域范围内应力作用具有较强的相关性；
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