2019年里奇克雷斯特破裂序列的动态,相互作用和延迟
Taufiq Taufiqurrahman1, Alice-Agnes Gabriel2,3, Duo Li1
1Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich, Germany.
Nature
|May 24, 2023
概括
我们为加利福尼亚地震开发了3D动态破裂模型, 我们的发现揭示了断层系统相互作用,流体和压力在地震动态中的关键作用,
科学领域:
- 地质学
- 计算地震学
- 地震物理
背景情况:
- 由于观测挑战和地震物理学的复杂性,地震危险评估历来依赖经验方法.
- 现有的数据驱动和基于物理的模型难以完全解释观测到的地震复杂性和动态行为.
研究的目的:
- 为加利福尼亚州2019年6.4级西尔斯山谷和7.1级里奇克雷斯特地震创建数据同化3D动态破裂模型.
- 研究连接这些大地震的物理机制, 了解复杂断层系统的动态.
主要方法:
- 使用超级计算机开发数据同化的三维动态破裂模型.
- 综合多样化的观测数据集,包括强运动,远地震,现场绘图,高速GPS和空间地质测量.
- 应用地震物理原理来解释观测到的地震和地质数据.
主要成果:
- 成功模拟了西尔斯山谷和里奇克雷斯特的地震序列,
- 确定区域结构,环境压力,断层系统相互作用,过压流体和低动态摩擦作为影响地震动态和延迟的关键因素.
- 证明了基于物理的模型能够协调密度地震记录和3D结构/应力数据.
结论:
- 基于物理和数据的联合方法对于理解复杂的断层系统和地震序列是有效的.
- 对广泛的观测数据的基于物理的解释对地质危险减缓策略具有变革潜力.
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