Options
Brogi, L.
Loading...
Preferred name
Brogi, L.
2 results
Now showing 1 - 2 of 2
- PublicationRestrictedMeMoVolc report on classification and dynamics of volcanic explosive eruptions(2016-10-28)
; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ; ;Bonadonna, C. ;Cioni, R. ;Costa, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia ;Druitt, T. ;Phillips, J. ;Pioli, L. ;Andronico, D.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia ;Harris, A. ;Scollo, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia ;Bachmann, O. ;Bagheri, G. ;Biass, S. ;Brogi ;Cashman, K. ;Dominguez, L ;Dürig, T. ;Galland, O. ;Giordano, G. ;Gudmundsson, M. ;Hort, M. ;Höskuldsson, A. ;Houghton, B. ;Komorowski, J. C. ;Küppers, U. ;Lacanna, G. ;Le Pennec, J. L. ;Macedonio, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia ;Manga, M. ;Manzella, I. ;de’ Michieli Vitturi, M. ;Neri, A. ;Pistolesi, M. ;Polacci, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Pisa, Pisa, Italia ;Ripepe, M. ;Rossi, E. ;Scheu, B. ;Sulpizio, R. ;Tripoli, B. ;Valade, S. ;Valentine, G. ;Vidal, C. ;Wallenstein, N. ; ;; ; ; ;; ;; ; ;; ; ; ; ; ; ; ; ; ; ; ; ; ; ;; ; ; ; ; ;; ; ; ; ; ; ; ; ;Classifications of volcanic eruptions were first introduced in the early twentieth century mostly based on qualitative observations of eruptive activity, and over time, they have gradually been developed to incorporate more quantitative descriptions of the eruptive products from both deposits and observations of active volcanoes. Progress in physical volcanology, and increased capability in monitoring, measuring and modelling of explosive eruptions, has highlighted shortcomings in the way we classify eruptions and triggered a debate around the need for eruption classification and the advantages and disadvantages of existing classification schemes. Here, we (i) review and assess existing classification schemes, focussing on subaerial eruptions; (ii) summarize the fundamental processes that drive and parameters that characterize explosive volcanism; (iii) identify and prioritize the main research that will improve the understanding, characterization and classification of volcanic eruptions and (iv) provide a roadmap for producing a rational and comprehensive classification scheme. In particular, classification schemes need to be objective-driven and simple enough to permit scientific exchange and promote transfer of knowledge beyond the scientific community. Schemes should be comprehensive and encompass a variety of products, eruptive styles and processes, including for example, lava flows, pyroclastic density currents, gas emissions and cinder cone or caldera formation. Open questions, processes and parameters that need to be addressed and better characterized in order to develop more comprehensive classification schemes and to advance our understanding of volcanic eruptions include conduit processes and dynamics, abrupt transitions in eruption regime, unsteadiness, eruption energy and energy balance.376 12 - PublicationOpen AccessMagnetotelluric measurements in the Monte Amiata region(1994-11)
; ; ; ; ; ; ;Manzella, A.; C.N.R., Istituto Internazionale per le Ricerche Geotermiche, Pisa, Italy ;Bellani, S.; C.N.R., Istituto Internazionale per le Ricerche Geotermiche, Pisa, Italy ;Brogi, L.; Dipartimento di Scienze della Terra, Università degli Studi di Pisa, Italy ;Jong, Q.; C.N.R., Istituto Internazionale per le Ricerche Geotermiche, Pisa, Italy ;Pinna, E.; Dipartimento di Scienze della Terra, Università degli Studi di Pisa, Italy ;Rossi, A.; C.N.R., Istituto Internazionale per le Ricerche Geotermiche, Pisa, Italy; ; ; ; ; A preliminary magnetotelluric (MT) survey was carried out in Southern Tuscany, Italy, to delineate the resistivity structure in an area which does not belong to classic geothermal zones but is still characterized by anomalously high heat flow. The one-dimensional (1D) resistivity inversion shows a low resistivity zone characterized by high heat flow. Based on 1D resistivity information, detailed two-dimensional (2D) resistivity modelling was carried out. A reasonable 2D resistivity model was proposed for shallow depths, and was found to be in good agreement with the available geological and geophysical information on the area. The present results show a low resistivity anomaly, characterized by high heat flow. The anomaly seems to extend beyond the classic Mt. Amiata geothermal region.164 185