Simplified structural scheme of the central Apennines inner zone, showing the main Quaternary normal faults (black lines, tick on downthrown side), Miocene-Pliocene thrusts (blue lines), the location of the M>5 events of the 2016-2017 seismic sequence, together with their focal mechanisms (available at http://cnt.rm.ingv.it/tdmt). The thin red lines are…
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Conduit stability effects on intensity and steadiness of explosive eruptions
Instability index versus mass discharge rate, for simulations performed with phonolitic, trachytic, dacitic and rhyolitic magmas (in titles). We present here results related to a set of simulations with variable values of inlet pressure (115–135 MPa) and water content (4.0–6.0 wt.% for phonolitic and trachytic magmas; and 4.5–6.5 wt.% for dacitic and rhyolitic…
Combined morphological and thermal analysis of lava flows: A way to boost understanding of emplacement dynamics
Figure 1Open in figure viewerPowerPointInput data: (a) shaded relief of the TINITALY DEM (Tarquini et al., 2012b) with the final July-August 2001 lava flows (modified after Behncke & Neri, 2003); (b) shaded relief of the 2004 LIDAR DEM (Mazzarini et al., 2005) over the DEM difference map…
Surface ruptures following the 30 October 2016 Mw 6.5 Norcia earthquake, central Italy
Civico R., S. Pucci, F. Villani, L. Pizzimenti, P. M. De Martini, R. Nappi & the Open EMERGEO Working Group (2018).
Journal of Maps, 14/2, 151-160, doi: 10.1080/17445647.2018.1441756
Identification of leveled archeological mounds (Höyük) in the alluvial plain of the Ceyhan River (Southern Turkey) by satellite remote-sensing analyses
Bini M., I. Isola, G. Zanchetta, A. Ribolini, A. Ciampalini, I. Baneschi, D. Mele, A.L. D’Agata (2018).
Remote sensing, 10/2, 241, ISSN: 2072-4292, doi: 10.3390/rs10020241
UAV-based remote sensing surveys of lava flow fields: a case study from Etna’s 1974 channel-fed lava flows
Favalli M., A. Fornaciai, L. Nannipieri, A. Harris, S. Calvari, C. Lormand (2018).
Bulletin of Volvanology, 80/3, https://doi.org/10.1007/s00445-018-1192-6.
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