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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author: Leonardo Sagnotti Fabio Speranza Alessandra Smedile Massimiliano Porreca Patrizia Macrì |
| Publication date | September 2016 |
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