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Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset.

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This study identifies optimal cell sizes (8-16 km) for complex network analysis of Norwegian earthquakes. It reveals that observational errors have minimal impact on network structure, ensuring stable seismic data interpretation.

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Area of Science:

  • Earth Sciences
  • Geophysics
  • Complex Networks

Background:

  • Intraplate earthquakes in southern Norway (1980-2020) are analyzed using complex network methods.
  • Defining appropriate spatial cell size is a critical challenge in complex network analysis of seismic data.

Purpose of the Study:

  • To investigate the influence of observational errors on complex network construction for Norwegian earthquakes.
  • To determine the optimal cell size for robust complex network analysis in this seismic region.

Main Methods:

  • Complex network analysis applied to intraplate earthquake data from southern Norway.
  • Examination of the degree distribution and critical exponent (γ) across varying cell sizes (2D and 3D networks).
  • Assessment of the impact of observational errors in hypocentral and epicentral locations.

Main Results:

  • Cell size significantly influences the critical exponent (γ) of the degree distribution.
  • Observational errors in location data showed a weak influence on the network's degree distribution.
  • Network structure transitions from hub-dominated (small cell size) to homogeneous (large cell size).

Conclusions:

  • A stable cell size range of 8 to 16 km is recommended for complex network studies in southern Norway.
  • The methodology provides a reliable basis for interpreting complex network structures in seismic regions.
  • The findings suggest that high-quality seismic data allows for stable complex network analysis, minimizing the impact of location uncertainties.