Abstract Characterizing the inelastic strain field around co-seismic faults is a key to understanding earthquake rupture processes. We aim to detect zones of inelastic deformation around surface ruptures, using Anisotropy of Magnetic Susceptibility (AMS) analyses. To characterize the paleo-seismic setting we measured 29 normal faults, which cut the late Pleistocene lacustrine Lisan Formation and were associated with shallow (

中文翻译：

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磁性织物检测到的表面破裂周围的非弹性变形区

摘要 表征同震断层周围的非弹性应变场是理解地震破裂过程的关键。我们的目标是使用磁化率各向异性 (AMS) 分析检测地表破裂周围的非弹性变形区域。为了表征古地震环境，我们测量了 29 个正断层，这些断层切割晚更新世湖相立三组并与浅层（