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Giuliana Mele, Emiliano Di Luzio and Cristina Di Salvo Mapping Moho depth variations in central Italy from PsMoho-P delay times: Evidence of an E-W transition in the Adriatic Moho at 42°N latitude Geochemistry, Geophysics, Geosystems 14

Version of Record online: 1 OCT 2013 | DOI: 10.1002/ggge.20235

Key Points

  • Delay of Moho conversions in central Italy are computed at 24 stations
  • Seismic stations are assigned to the Adriatic and peri-Tyrrhenian crust
  • An E-W oriented transition in the Adriatic Moho is inferred

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