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CORDIS

Strain Localisation in Magma

Ziel

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.

Aufforderung zur Vorschlagseinreichung

ERC-2012-StG_20111012
Andere Projekte für diesen Aufruf anzeigen

Gastgebende Einrichtung

THE UNIVERSITY OF LIVERPOOL
EU-Beitrag
€ 1 908 000,00
Adresse
BROWNLOW HILL 765 FOUNDATION BUILDING
L69 7ZX Liverpool
Vereinigtes Königreich

Auf der Karte ansehen

Region
North West (England) Merseyside Liverpool
Aktivitätstyp
Higher or Secondary Education Establishments
Hauptforscher
Yan Lavallée (Dr.)
Kontakt Verwaltung
Janette Ryan (Mrs.)
Links
Gesamtkosten
Keine Daten

Begünstigte (1)