作者: Marco Nocentini , Riccardo Asti , Domenico Cosentino , Federica Durante , Elsa Gliozzi
DOI: 10.1080/17445647.2017.1340910
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摘要: ABSTRACTWe present a geological map at 1:25,000 scale of the Plio-Quaternary L’Aquila-Scoppito intermontane basin (central Italy), which corresponds to epicentral area 6th April 2009 L’Aquila earthquake (Mw: 6.29). The is derived from field surveys 1:5000 and takes into account previously published maps. It supported by fine-scale LiDAR digital elevation model, paleontological analyses, 14C dating, well log analyses deep boreholes, geophysical data interpretation. By taking that remarkable historical present-day seismicity result its evolution, aim this study produce through comprehensive analysis occurring synthems tectonic processes are place within it.