本文论述北京地区的断层活动特征,着重讨论断层活动的阶段性变化。
The fault activities in Beijing region show a changing feature by stages.
依据分形理论分析了活动断裂带内断裂系、水系及断层泥粒度分布的分形结构特征。
On the basis of fractal theory, the fractal structure features of fracture systems, water systems and granulometric distributions of fault gouges in the active fault zones are analyzed.
构造地貌能反映断裂的结构变形特征和断层的活动强度。例如断层陡坎的高度、长度和坡度以及断层陡坎的连续程度。
Tectonic topography can reflect the structural deformation feature and active strength of faults, such as the height, length and gradient of a fault scarp as well as its continuity.
在这篇文章结尾,还讨论了冲洪积扇特征对断层活动强度的反映。
At the end of this paper, we discussed the reflection of alluvial fan on the active strength of faults.
详细的卫星图像分析和野外调查表明活动断层(开都河断层带)主要分布在盆地的南缘,具典型的走滑断层特征。
Detailed analyses of satellite images and field investigation have revealed that the active Kaidu River fault zone on the southern margin of the basin is a strike-slip fault zone.
主要活动断层和活动断块分别控制上列滑坡带和滑坡区的分布,其活动特征、断距和长度大小分别决定了沿线多数滑坡的分布规律、发育程度和规模大小。
These landslide belts and districts are mainly controlled by the active faults and blocks in Weihe rift valley at most points, such as the distribution, the scale and the development degree.
茨湖断层具有最新活动特征,粘滑标志明显。
The Cihu Fault in the region is recently active, its feature of stick slip is clear.
通过ETM卫星影像和野外考察分析了工程引水隧洞线路区断层的空间分布及活动特征。
Through ETM and exploring in site, analyze the distribution and the activity of active faults, evluate faults influences on the stability of deeply buried long tunnel.
断层泥是断层活动的信息载体,其中的石英颗粒微形貌特征能够反映断层活动年代、活动方式。
Gouge is an information carrier for fault activity, and the motion mode and date of the fault activity can be identified by observation of micro-shape characteristics of quartz in the gouges.
讨论了隐伏断层挽近活动特征及其对地下水补径排条件的影响。
The distribution of hidden movements faults and supplement, runoff and draining of groundwater in Minle basin in front of the Qilian Mountain is studied in this paper.
葡萄花油层断层具有密集成带特征,且密集带边界断层多为成藏期活动的油源断层;
Putaohua reservoir fault have a dense like banding characteristics, and more boundary fault of dense banding are oil source fault activities for the accumulation period;
断层泥是断层活动的信息载体,其中的石英颗粒微形貌特征能够反映断层活动方式、期次和活动年代。
Gouge is an information carrier for fault activity. The motion mode and date of the fault activity can be identified by observation of micro-shape characteristics of quartz in the gouges.
断层泥是断层活动的信息载体,其中的石英颗粒微形貌特征能够反映断层活动方式、期次和活动年代。
Gouge is an information carrier for fault activity. The motion mode and date of the fault activity can be identified by observation of micro-shape characteristics of quartz in the gouges.
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