地震学:桑达河沟的地震风险
Suleyman S Nalbant1, Sandy Steacy, Kerry Sieh
1School of Environmental Sciences, University of Ulster, Coleraine, County Derry BT52 1SA, UK.
Nature
|June 10, 2005
概括
2005年苏丹大地震是由2004年苏门答腊-安达曼事件引发的. 这种地震活动增加了南部巨型冲压的压力,使其成为未来地震的候选人.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 2005年3月28日,在2004年12月发生类似事件之后,桑达大震区经历了一次大地震.
- 这次2005年的裂与2004年苏门答腊-安达曼地震有空间联系.
研究的目的:
- 调查2005年苏丹大地震发生后的触发机制和应力转移.
- 评估相邻的巨大冲击部分和断层的地震潜力.
主要方法:
- 对2005年地震的地震数据的分析.
- 应力建模用于计算附近构造结构的应力变化.
- 对Mentawai部分的古地震数据的审查.
主要成果:
- 2005年的地震是由非常小的应力 (约0.1巴) 引发的.
- 断裂增加了断裂区域以南的大压力,靠近巴图和门塔瓦伊岛屿.
- 在苏门答腊断层上也观察到压力增加.
- 古地震证据表明,Mentawai部分处于其地震周期的后期阶段.
结论:
- 2005年的桑达大地震是2004年地震压力转移的结果.
- 桑达大震区的Mentawai部分由于其先进的地震周期,非常容易受到未来引发的地震的影响.
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