1887

Abstract

Summary

The recent seismic data offshore Greece revealed, south of Crete, the presence of an external Hellenides carbonate unit similar in dimensions to this of the island of Crete. Velocity modelling helps in this study to emphasise the tectonic-stratigraphic image below the seafloor at depths reaching 9 kilometres.

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/content/papers/10.3997/2214-4609.201803050
2018-12-06
2024-03-29
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References

  1. Bohnhoff, M., H. P.Harjes, and T.Meier
    , 2005, Deformation and stress regimes in the Hellenic subduction zone from focal mechanisms: Journal of Seismology, v. 9, no.3), p. 341–366.
    [Google Scholar]
  2. Gallen, S. F., K. W.Wegmann, D. R.Bohnenstiehl, F. J.Pazzaglia, M. T.Brandon and C.Fassoulas,
    , 2014, Active simultaneous uplift and margin-normal extension in a forearc high, Crete, Greece: Earth and Planetary Science Letters, v. 398, p. 11–24.
    [Google Scholar]
  3. Kopf, A., J.Mascle, D.Klaeschen
    , 2003, The Mediterranean Ridge: A mass balance across the fastest growing accretionary complex on Earth: Journal of Geophysical Research, v. 108, no. B8, p. 2372.
    [Google Scholar]
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