EARTHCRACKS

Laboratory earthquakes: dynamic shear cracks in heterogeneous frictional interfaces

 Coordinatore UNIVERSITETET I OSLO 

 Organization address address: Problemveien 5-7
city: OSLO
postcode: 313

contact info
Titolo: Ms.
Nome: Trine-Lise
Cognome: Knudsen
Email: send email
Telefono: -22856388
Fax: -22855054

 Nazionalità Coordinatore Norway [NO]
 Totale costo 0 €
 EC contributo 212˙729 €
 Programma FP7-PEOPLE
Specific programme "People" implementing the Seventh Framework Programme of the European Community for research, technological development and demonstration activities (2007 to 2013)
 Code Call FP7-PEOPLE-IEF-2008
 Funding Scheme MC-IEF
 Anno di inizio 2009
 Periodo (anno-mese-giorno) 2009-03-01   -   2011-02-28

 Partecipanti

# participant  country  role  EC contrib. [€] 
1    UNIVERSITETET I OSLO

 Organization address address: Problemveien 5-7
city: OSLO
postcode: 313

contact info
Titolo: Ms.
Nome: Trine-Lise
Cognome: Knudsen
Email: send email
Telefono: -22856388
Fax: -22855054

NO (OSLO) coordinator 212˙729.11

Mappa

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collaborations    scheibert    friction    dr    dynamics    fracture    experts    earthquake    experimental    data    physics    interface    disciplinary    pgp   

 Obiettivo del progetto (Objective)

'The main objective of the proposal is to expose an outstanding young experimental physicist to multidisciplinary research on earthquake dynamics. Dr. Julien Scheibert who is already an expert in friction and fracture dynamics will perform original research and receive training at the Norwegian Centre of Excellence, “Physics of Geological Processes” (PGP) at the University of Oslo. By working with geologists and physicists with a proven record of cross disciplinary research Dr. Scheibert will broaden his competences and reach a deeper level of insight into fracture and friction in Nature. The main methods to be applied are novel model experiments in which a highly controlled disorder is introduced at a frictional elastomer-on-glass multicontact interface mimicking a seismic fault and correlated to the dynamics of both the nucleation and propagation phases of a shear crack. The dynamics of the slip field over the whole interface will be monitored optically using high speed camera acquisition and digital image correlation techniques. The acoustic signals emitted during rupture will be registered simultaneously by broadband transducers. The experimental data will be compared with earthquake field data, continuum and discrete modelling and theoretical approaches in collaborations with experts at PGP. This project should strengthen a multi-disciplinary approach to seismology in Europe, by gathering experts in geosciences, statistical physics and mechanical engineering and promote new collaborations between them.'

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