Extension fracture due to collinear cracks

Golecki, J. J.; Ornai, David

doi:10.1016/0013-7944(95)00168-9

Cited by 2 publications

(1 citation statement)

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“…Interactions between double fractures were then investigated in analytical solutions[9]. Only two collinear fractures were considered in these studies[10]. However, analytical solutions are too simple for real geologic conditions and are not suitable for noncollinear fractures.…”

Section: Introductionmentioning

confidence: 99%

The interactions of fault patterns and stress fields during active faulting in Central North China Block: Insights from numerical simulations

Hou

2019

PLoS ONE

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The interaction of active faults as a factor affecting the mechanisms of large earthquakes has been observed in many places. Most aftershock and clustering earthquake sequences do not recur on the main seismogenic fault but are controlled by fault interactions with adjacent seismic structures. Four groups of conceptual models were generated in this study to determine how the geometry of the seismogenic faults controls the distributions of stress fields and earthquakes. The influences of the fault length ratio, center distance, overlap ratio, echelon distance and fault opening angle were considered in a 2D viscoelastic model. The results indicate that the interaction in the slipping zone is larger when collinear interacting faults are more closely positioned, with one fault lengthening. For noncollinear faults, the interaction is stronger as the inner tips pass each other, which impedes their growth after some degree of overlap. Additionally, fault interaction at the slipping zone becomes stronger as the opening angle approaches 180°. We further generated a 3D viscoelastic model of fault interactions in Central North China Block and applied the finite element method to analyze the relationship between distributions of earthquakes and fault geometry. The calculated results reveal well-matched higher stress and maximum shear strain concentrations in the southern part of the Fen-wei Graben Zone than in other zones in Central North China Block, which can be explained by the longer faults, shorter center distances, shorter overlap lengths and larger opening angles. The stress distributions and fault interactions should be considered in long-term seismic hazard assessment in these zones.

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Section: Introductionmentioning

confidence: 99%