Archivio News Toward continuous quantification of lava extrusion rate: Results from the multidisciplinary analysis of the 2 January 2010 eruption of Piton... Quantifying volcanic hazard at Campi Flegrei caldera (Italy) with uncertainty assessment: 2. Pyroclastic density current invasion maps Quantifying volcanic hazard at Campi Flegrei caldera (Italy) with uncertainty assessment: 1. Vent opening maps A detailed analysis of wastewater‐induced seismicity in the Val d’Agri oil field (Italy) Late Pleistocene-Holocene volcanic activity in northern Victoria Land recorded in Ross Sea (Antarctica) marine sediments The origin of along-rift variations in faulting and magmatism in the Ethiopian Rift Disperse Two-Phase Flows, with Applications to Geophysical Problems Complex dynamics of small-moderate volcanic events: the example of the 2011 rhyolitic Cordón Caulle eruption, Chile « Previous 1 … 39 40 41 42 43 Next »
![(a) Three-dimensional locations (dots) of the 2005–2006 seismicity recorded in VA by the INGV temporary network (blue triangles) and Vp model at 3 km depth. Cyan triangles denote INGV permanent stations, white squares the productive wells, while the black square the CM2 well. The yellow dashed line outlines the Quaternary basin. (b) Vp and Vp/Vs sections across the swarm induced by the CM2 well (yellow dots) and the cluster induced by the water impoundment (red dots). Quaternary normal faults bounding the basin to the SW (NE dipping, blue lines) and NE (SW dipping, black lines) are redrawn from Valoroso et al. [2011].](https://www.pi.ingv.it/wp-content/uploads/2015/04/GRL_Improta_etal_Fig1m.png)
