首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Finite element simulations of dynamic shear rupture experiments and dynamic path selection along kinked and branched faults
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Finite element simulations of dynamic shear rupture experiments and dynamic path selection along kinked and branched faults

机译:动态剪切断裂实验的有限元模拟和沿扭折和分支断层的动态路径选择

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We analyze the nucleation and propagation of shear cracks along nonplanar, kinked, and branched fault paths corresponding to the configurations used in recent laboratory fracture studies by Rousseau and Rosakis (2003, 2009). The aim is to reproduce numerically those shear rupture experiments and from that provide an insight into processes which are active when a crack, initially propagating in mode II along a straight path, interacts with a bend in the fault or a branching junction. The experiments involved impact loading of thin Homalite-100 (a photoelastic polymer) plates, which had been cut along bent or branched paths and weakly glued back together everywhere except along a starter notch near the impact site. Strain gage recordings and high-speed photography of isochromatic lines provided characterization of the transient deformation fields associated with the impact and fracture propagation. We found that dynamic explicit 2-D plane-stress finite element analyses with a simple linear slip-weakening description of cohesive and frictional strength of the bonded interfaces can reproduce the qualitative rupture behavior past the bend and branch junctions in most cases and reproduce the principal features revealed by the photographs of dynamic isochromatic line patterns. The presence of a kink or branch can cause an abrupt change in rupture propagation velocity. Additionally, the finite element results allow comparison between total slip accumulated along the main and inclined fault segments. We foundthat slip along inclined faults can be substantially less than slip along the main fault, and the amount depends on the branch angle and kink or branch configuration.
机译:我们分析了沿非平面,扭结和分支断层路径的剪切裂纹的成核和扩展,这些路径对应于最近由Rousseau和Rosakis(2003,2009)进行的实验室断裂研究中使用的配置。目的是从数值上再现那些剪切断裂实验,并从中提供洞察力,当裂纹最初以II型沿直线路径传播,与断层或分支结中的弯曲相互作用时,这些过程将起作用。实验涉及薄薄的Homalite-100(光弹性聚合物)板的冲击载荷,该板沿弯曲或分支的路径被切割,并且除了沿冲击部位附近的起动器缺口外,在各处无力地胶粘在一起。应变计记录和等色线的高速摄影提供了与冲击和裂缝扩展相关的瞬态变形场的特征。我们发现,通过对键合界面的内聚力和摩擦强度进行简单线性滑弱描述的动态显式二维平面应力有限元分析,在大多数情况下可以重现弯曲和分支结点的定性断裂行为,并重现主要原理。动态等色线图案照片揭示的特征。扭结或分支的存在会导致破裂传播速度的突然变化。另外,有限元结果允许在沿主断层段和倾斜断层段累积的总滑动之间进行比较。我们发现,沿倾斜断层的滑动远小于沿主要断层的滑动,其数量取决于分支角度和扭结或分支构型。

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