从西苏门答腊的珊瑚中记录的海平面变化推断出地震超级周期
Kerry Sieh1, Danny H Natawidjaja, Aron J Meltzner
1Tectonics Observatory, California Institute of Technology, Pasadena, CA 91125, USA. sieh@ntu.edu.sg
概括
来自门塔瓦伊群岛的珊瑚记录显示,桑达大压力每200年就会产生一次大地震. 2007年的地震是该地震区预期出现的几个部分故障中的第一个.
科学领域:
- 地质地质地质地质地质地
- 古代地震学 (paleoseismology) 是一种古地震学.
- 构造学 构造学 构造学 构造学
背景情况:
- 桑达大冲压 (Sunda megathrust) 是一个主要的构造特征,在印度尼西亚负责显著的地震活动.
- 了解大地震的复发间隔对于评估该地区的地震危险至关重要.
研究的目的:
- 为了重建沿着桑达大震区的Mentawai部分的大地震的历史.
- 评估该部分的地震潜力和未来破裂行为.
主要方法:
- 在珊瑚群中保存的相对海平面变化记录的分析.
- 基于珊瑚样本的地球时间学数据的古地震重建.
主要成果:
- 有证据表明,在过去的700年里,大地震的重复间隔约为200年.
- 2007年8.4级地震被确定为一系列潜在的破裂事件中的初始事件.
结论:
- 桑达大震区的Mentawai部分表现出一个一致的模式,产生了巨大的地震.
- 2007年地震可能标志着部分故障的多十年序列的开始,需要持续监测和危险评估.
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