在秘鲁中部的巨大冲击中发生的地震和无地震滑动
Hugo Perfettini1, Jean-Philippe Avouac, Hernando Tavera
1Institut de Recherche pour le Développement, 44 Boulevard de Dunkerque, 13572 Marseille cedex 02, France. hugo.perfettini@ird.fr
Nature
|May 7, 2010
概括
地震和无地震滑动在俯冲巨型冲击上适应板块运动. 在秘鲁中部,无地震滑动占滑动的70%,影响地震的频率和强度.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 俯冲巨型冲击物表现出地震 (地震) 和无地震 (爬行) 滑动模式.
- 这些滑动模式相互作用,以适应长期板块构造运动.
- 浅层的大冲压区域显示异质的应变,表明两种滑动类型的共存.
研究的目的:
- 研究秘鲁中部巨型岩层上的地震和无地震滑动之间的相互作用.
- 了解无地震爬行如何影响大地震的发生和特征.
- 分析地质特征的作用,如纳斯卡山脊,调节滑动行为.
主要方法:
- 皮斯科地震 (Mw = 8.0) 破裂过程的分析.
- 间地震和后地震变形的建模.
- 识别度和无地震后滑位的识别.
主要成果:
- 皮斯科地震破裂了锁定的度,并触发了邻近地区的无地震后滑坡.
- 纳斯卡山脊的俯冲区域显示了较低的地震间合,并充当了破裂屏障.
- 与无地震滑动相关的增速补丁,控制地震的范围和频率.
结论:
- 秘鲁中部的大冲压包括交替减弱速度 (地震) 和增强速度 (无地震) 的补丁.
- 无地震滑坡占滑坡总预算的很大一部分 (50-70%).
- 据估计,Pisco地区Mw = 8.0地震的回归期约为250年.
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