首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Bookshelf Kinematics and the Effect of Dilatation on Fault Zone Inelastic Deformation: Examples From Optical Image Correlation Measurements of the 2019 Ridgecrest Earthquake Sequence
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Bookshelf Kinematics and the Effect of Dilatation on Fault Zone Inelastic Deformation: Examples From Optical Image Correlation Measurements of the 2019 Ridgecrest Earthquake Sequence

机译:书架运动学及扩张对故障区无弹性变形的影响:2019脊古典地震序列光学图像相关测量的实例

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The 2019 Ridgecrest earthquake sequence initiated on July 4th with a series of foreshocks, including an M-w 6.4 event, that culminated a day later with the M-w 7.1 mainshock and resulted in rupture of a set of cross-faults. In this study, we use subpixel correlation of optical satellite imagery to measure the displacement, finite strain, and rotation of the near-field coseismic deformation to understand the kinematics of strain release along the surface ruptures. We find the average off-fault deformation along the mainshock rupture is 34% and is significantly higher along the foreshock rupture (56%), suggesting it is a less structurally developed fault system. Measurements of the 2D dilatational strain along the mainshock rupture show a dependency of the width of inelastic strain with the degree of fault extension and contraction, indicating wider fault zones under extension than under shear. Measurements of the vorticity along the main, dextral rupture show that conjugate sinistral faults are embedded within zones of large clockwise rotations caused by the transition of strain beyond the tips of dextral faults leading to bookshelf kinematics. These rotations and bookshelf slip can explain why faults of different shear senses do not intersect one another and the occurrence of pervasive and mechanically unfavorable cross-faulting in this region. Understanding the causes for the variation of fault zone widths along surface ruptures has importance for reducing the epistemic uncertainty of probabilistic models of distributed rupture that will, in turn, provide more precise estimates of the hazard distributed rupture poses to nearby infrastructure.
机译:2019年山脊地震序列始于7月4日,伴随着一系列前震,包括一次M-w 6.4事件,一天后以M-w 7.1主震达到高潮,并导致一组交叉断层破裂。在本研究中,我们使用光学卫星图像的亚像素相关性来测量近场同震形变的位移、有限应变和旋转,以了解沿地表破裂释放应变的运动学。我们发现,沿主震断裂的平均离断层变形为34%,沿前震断裂的平均离断层变形显著更高(56%),表明它是一个结构较不发达的断层系统。沿主震破裂的二维膨胀应变测量表明,非弹性应变的宽度与断层伸展和收缩的程度有关,表明伸展下的断层带比剪切下的断层带更宽。沿主右旋断裂的涡度测量表明,共轭左旋断层嵌入在大型顺时针旋转区域内,该区域由右旋断层尖端以外的应变过渡引起,导致书架运动学。这些旋转和书架滑动可以解释为什么不同剪切感的断层彼此不相交,以及该地区普遍存在的机械上不利的交叉断层。了解断层带宽度沿地表破裂变化的原因,对于减少分布式破裂概率模型的认知不确定性具有重要意义,而分布式破裂概率模型反过来将提供对附近基础设施的危险性的更精确估计。

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