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Regularized inversion for coseismic slip distribution with active constraint balancing

机译:具有主动约束平衡的同震滑动分布正则化反演

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摘要

Estimating the spatial distribution of coseismic slip is an ill-posed inverse problem, and solutions may be extremely oscillatory due to measurement errors without any constraints on the coseismic slip distribution. In order to obtain stable solution for coseismic slip inversion, regularization method with smoothness-constrained was imposed. Trade-off parameter in regularized inversion, which balances the minimization of the data misfit and model roughness, should be a critical procedure to achieve both resolution and stability. Then, the active constraint balancing approach is adopted, in which the trade-off parameter is regarded as a spatial variable at each model parameter and automatically determined via the model resolution matrix and the spread function. Numerical experiments for a synthetical model indicate that regularized inversion using active constraint balancing approach can provides stable inversion results and have low sensitivity to the knowledge of the exact character of the Gaussian noise. Regularized inversion combined with active constraint balancing approach is conducted on the 2005 Nias earthquake. The released moment based on the estimated coseismic slip distribution is 9.91×1021N·m, which is equivalent to a moment magnitude of 8.6 and almost identical to the value determined by USGS. The inversion results for synthetic coseismic uniform-slip model and the 2005 earthquake show that smoothness-constrained regularized inversion method combined with active constraint balancing approach is effective, and can be reasonable to reconstruct coseismic slip distribution on fault.
机译:估计同震滑动的空间分布是一个不适当地的逆问题,由于测量误差而对同震滑动分布没有任何限制,因此解决方案可能会非常振荡。为了获得同震滑动反演的稳定解,提出了一种受光滑度约束的正则化方法。平衡数据最小化和模型粗糙度的平衡的正则化反演中的折衷参数应该是实现分辨率和稳定性的关键过程。然后,采用主动约束平衡方法,其中权衡参数被视为每个模型参数的空间变量,并通过模型分辨率矩阵和扩展函数自动确定。合成模型的数值实验表明,使用主动约束平衡方法的正则化反演可以提供稳定的反演结果,并且对高斯噪声的精确特征的认识敏感性较低。对2005年的尼亚斯地震进行了正则反演与主动约束平衡法相结合。基于估计的同震滑动分布的释放力矩为9.91×1021N·m,相当于力矩大小8.6,几乎与USGS确定的值相同。综合同震均匀滑动模型和2005年地震的反演结果表明,结合约束约束的光滑度正则化反演方法是有效的,可以合理地重建断层同震滑动分布。

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  • 来源
    《中南大学学报(英文版)》 |2017年第12期|2961-2968|共8页
  • 作者单位

    School of Geosciences and Info-physics, Central South University, Changsha 410083, China;

    School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia V8P 5C2, Canada;

    School of Geosciences and Info-physics, Central South University, Changsha 410083, China;

    School of Earth and Ocean Sciences, University of Victoria, Victoria, British Columbia V8P 5C2, Canada;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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  • 入库时间 2022-08-18 01:06:27
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