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首页> 外文期刊>Earthquake Research in China >The Grouping of the Strike-Slip Offset Data and Its Relation with The Seismicity Along Middle Segment Of the Xiaojiang Active Fault
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The Grouping of the Strike-Slip Offset Data and Its Relation with The Seismicity Along Middle Segment Of the Xiaojiang Active Fault

机译:小江活动断裂中段走滑偏移量数据的分组及其与地震活动的关系

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摘要

The data of the strike-slip offset along the Xiaojiang active fault can be obviously grouped. The groups of small orders of magnitude data within 100 m show clear linear characteristics of increments between 8 m and 12 m, which indicates that the segments of the Xiaojiang active fault is of characteristic seismicity and the distribution of the values of each group indicates that there are smaller earthquakes and creep between two large earthquakes along each segment of the Xiaojiang active fault. The interval between two characteristic large earthquakes can be calculated with the increments for two groups of slip data and the slip rate of the fault.
机译:沿小江活动断裂带走滑偏移的数据可以明显地分组。 100 m范围内的小量级数据组显示出清晰的线性特征,其增量在8 m和12 m之间,这表明小江活动断层的分段具有特征地震活动性,并且每组值的分布表明是较小的地震,以及沿着小江活动断裂带各段的两次大地震之间的蠕变。可以利用两组滑动数据和断层滑动率的增量来计算两次特征性大地震之间的间隔。

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