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Variability of repeating earthquake behavior along the Longitudinal Valley fault zone of eastern Taiwan

机译:台湾东部纵谷断裂带重复地震行为的变异性

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摘要

Two major clusters of repeating earthquake sequences (RES) are found on two fault patches near the Longitudinal Valley fault (LVF) in eastern Taiwan, the Chihshang segment to the south and the Hualien segment to the north. The 25 M2.3-4.6 RES on the Hualien segment are widely distributed in a NNE direction over a distance of 45 km, whereas on the Chihshang segment, the 30 M 2.2-3.4 RES have a shorter along-strike extent of about 15 km. The longer spatial extent of RES on the Hualien segment may indicate a wider distributed creeping zone at depth. M > 3.8 RES are observed on the Hualien segment and are characterized by quasiperiodic recurrence. Statistical analysis of the size and number of earthquakes adjacent to the RES indicates that the smaller number of large earthquakes in the vicinity may explain the quasiperiodic recurrence of RES. We argue that on the Hualien segment, M-4 or larger earthquakes are isolated enough in space to facilitate the occurrence of repeated ruptures.
机译:在台湾东部的长谷断裂带(LVF)附近的两个断裂斑片上发现了两个主要的重复地震序列簇(RES),南部的赤上段和北部的花莲段。花莲段上的25 M2.3-4.6 RES在NNE方向上广泛分布于45 km的距离上,而在池上段上,30 M 2.2-3.4 RES的沿走向范围较短,约为15 km 。花莲段上RES的空间范围越长,表明深处的蠕变带越宽。在花莲段上观测到M> 3.8 RES,其特征是拟周期性复发。对RES附近地震的规模和数量的统计分析表明,附近较小的大地震数量可以解释RES的准周期性复发。我们认为在花莲段上,M-4或更大的地震在空间上足够孤立,以利于反复破裂的发生。

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