Roberto Isaia

TL;DR: In this paper, a detailed stratigraphical, structural, volcanological and 14 C (AMS) geochronological study devoted to the reconstruction of the volcanic and deformational history of the Campi Flegrei caldera was carried out.

TL;DR: In this article, the authors performed forecasting and hazard assessment at the restless Campi Flegrei caldera, within the Neapolitan volcanic area, using stratigraphical, volcanological, structural and petrological data.

TL;DR: Wulf et al. as mentioned in this paper used a database of proximal glass compositions to correlate proximal volcanic deposits through to distal tephra layers in the Lago di Monticchio record and these correlations provide information on eruption stratigraphy and the tempo of volcanism at Campi Flegrei.

TL;DR: In this article, geochronological, geochemical, and Sr-isotope data on volcanics erupted before the Campanian Ignimbrite (CI, 37 ka) and the Neapolitan Yellow Tuff (NYT, 12 ka) caldera-forming eruptions at Campi Flegrei (CF) have allowed us to investigate the behavior and temporal evolution of the Phlegraean magmatic system.

TL;DR: In this article, the authors performed an analysis of the ground deformation and seismic data collected since 1970 and showed that the detected deformation can be accounted for by an overpressure of 75 MPa in a source with a radius of 1 km, located at 5 km depth.