苏门答腊岛北部近代地震活动的时空条件

Elkawnie Pub Date : 2021-07-19 DOI:10.22373/ekw.v7i1.8797
I. Nurana, A. Simanjuntak, M. Umar, D. C. Kuncoro, S. Syamsidik, Y. Asnawi
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引用次数: 5

摘要

利用古腾堡-里希特关系可以统计分析地震易发区的应力状况和近期地震活动性。我们将此关系应用于苏门答腊岛北部1970-2020年M≥4、深度≤200 km的震源分布。在空间上,a值和b值反映了俯冲系统界面带和Seulimeum断裂北段构造致密的横向非均质性和应力聚集。在时间上,这两个区域都表现出缓慢的破坏周期和地震间隙,在具有高地震参数值的特定簇中具有高应力积累。时空分析结果表明,每次大地震发生前通常有一个较低的统计参数值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial Temporal Condition of Recent Seismicity In The Northern Part of Sumatra
The condition of stress and recent seismicity in the seismic-prone area can be statistically analyzed with the Gutenberg-Richter relation. We apply this relation to the hypocenter distribution for the period 1970-2020 with M ≥ 4 and depth ≤ 200 km  in the northern part of Sumatra. Spatially, The results obtained, a-values and b-values, figure a lateral heterogeneity and stress accumulation with dense structures at the interface zone in the subduction system and the northern segmentation of the Seulimeum fault. In time, both zones illustrate a slow time-to-failure cycle and seismic gap with high stress accumulation in the specific clusters with high seismic parameter values. The results of the spatial temporal analysis illustrate that each major earthquake event is usually preceded by a low statistical parameter value.
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