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March 3, 2026TectonophysicsOpen Access

P-wave seismic interferometric profile within the Granada Basin (Southern-Spain)

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Authors

CAC. Araque-PérezDSD. StichTTT. Teixido

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Overview

Observational analysis reveals complex crustal structure in the Granada Basin, suggesting tectonic activity implications.

Key Points

  • The resulting seismic section shows deep crustal features, including a low-angle detachment at 10–15 km depth.
  • Analysis incorporates data from 117 earthquakes across 44 km and 3 seismic stations over 40 years.
  • Seismic interferometry enhances subsurface illumination and reflector continuity despite sparse data collection.
  • Integration with local seismicity supports interpretations of crustal faults and basin structure.

Cite This Study

Araque-Pérez et al. (2026) studied this question.

synapsesocial.com/papers/69a7606cc6e9836116a2d26ahttps://doi.org/10.1016/j.tecto.2026.231114
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