SLIM
Strain Localisation in Magma
| Coordinatore | THE UNIVERSITY OF LIVERPOOL
Spiacenti, non ci sono informazioni su questo coordinatore. Contattare Fabio per maggiori infomrazioni, grazie. |
| Nazionalità Coordinatore | United Kingdom [UK] |
| Totale costo | 1˙908˙000 € |
| EC contributo | 1˙908˙000 € |
| Programma | FP7-IDEAS-ERC
Specific programme: "Ideas" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013) |
| Code Call | ERC-2012-StG_20111012 |
| Funding Scheme | ERC-SG |
| Anno di inizio | 2012 |
| Periodo (anno-mese-giorno) | 2012-10-01 - 2017-09-30 |
Partecipanti
| # | ||||
|---|---|---|---|---|
| 1 |
THE UNIVERSITY OF LIVERPOOL
Organization address
address: Brownlow Hill, Foundation Building 765 contact info |
UK (LIVERPOOL) | hostInstitution | 1˙908˙000.00 |
| 2 |
THE UNIVERSITY OF LIVERPOOL
Organization address
address: Brownlow Hill, Foundation Building 765 contact info |
UK (LIVERPOOL) | hostInstitution | 1˙908˙000.00 |
Mappa
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Obiettivo del progetto (Objective)
'The tendency of geomaterials to localise deformation is a measure of “the fragility of the Earth” – a threshold to the occurrence of geological hazards. At volcanoes, the remarkable, unpredictable and alarming occurrence of eruptions, switching from low-risk effusive to high-risk explosive eruptive behaviour is a direct consequence of strain localisation in magma (SLiM).
A deformation mechanism map of magma subjected to strain localisation will allow numerical models with higher accuracy, which, coupled to an understanding of the mechanics driving the monitored geophysical signals precursor to failure, will enhance eruption forecasts.
We propose a truly innovative and interdisciplinary approach to a description of SLiM. This collaborative study will pioneer in the integration of efforts from field geologists, experimentalist, mineralogists, petrologists, seismologists, and numerical modellers to underline the effects of microscopic processes responsible for the large-scale impacts of strain localisation in magma during transport and eruption.'