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      Analysis of a 150 m sediment core from the co-seismic subsidence depocenter of the 2009 Mw = 6.1 L'Aquila earthquake (Italy): Implications for Holocene-Pleistocene tectonic subsidence rates and for the age of the seismogenic Paganica fault system

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      Tectonophysics
      Elsevier BV

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          Journal
          Tectonophysics
          Tectonophysics
          Elsevier BV
          00401951
          September 2016
          September 2016
          : 687
          : 180-194
          Article
          10.1016/j.tecto.2016.09.004
          aa3c1d1e-4eaa-46e1-9697-5a1a1d97088a
          © 2016

          https://www.elsevier.com/tdm/userlicense/1.0/

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