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Data Acquisition Protocol for Determining Embedded Sensitivity Functions
Published on: April 20, 2016
2004年12月26日发生的苏门答腊 - 安达曼大地震
Thorne Lay1, Hiroo Kanamori, Charles J Ammon
1Earth Sciences Department, University of California, Santa Cruz, CA 95064, USA.
概括
2004年和2005年的苏门答腊 - 安达曼地震涉及重大断层滑动. 北部部分发生了缓慢滑动事件,影响了海的动态.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 津波科学 津波科学 津波科学
背景情况:
- 2004年印度洋地震 (Mw 9.19.3) 和2005年余震 (Mw 8.6) 是40年来最大的地震.
- 这些事件破裂了印度-澳大利亚/欧亚板边界的1600公里段.
- 2004年地震引发了一场毁灭性的海,造成超过283,000人死亡.
研究的目的:
- 分析2004年和2005年巨型地震的空间和时间滑坡分布.
- 为了研究北断区缓慢滑动的发生和特征.
主要方法:
- 分析地震和地测数据以建模地震破裂过程.
- 海建模和观测分析,以了解波浪的产生和传播.
- 沿断层边界不同段的滑动行为的比较.
主要成果:
- 在苏门答腊邦达阿切附近观察到严重的断层滑动 (高达15米).
- 沿尼科巴尔和安达曼群岛段发生了较小的快速滑落.
- 有证据表明,在北段有相当大的缓慢滑动 (分钟到小时).
结论:
- 2004/2005年苏门答腊-安达曼地震表现出异质的滑动,南部和北部部分之间存在差异.
- 缓慢滑动过程在北部断裂区中发挥了重要作用,可能影响海产生和地震危险.
- 了解异质滑动和缓慢滑动对于准确的地震和海危险评估至关重要.
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