Opendata, web and dolomites

DAMAGE SIGNED

seismic off-fault Deformation: A multi-scale iMAGing to constrain Earthquake energy budget

Total Cost €

0

EC-Contrib. €

0

Partnership

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 DAMAGE project word cloud

Explore the words cloud of the DAMAGE project. It provides you a very rough idea of what is the project "DAMAGE" about.

rock    faults    egrave    deformation    alpes    datasets    conceived    professional    represented    ruptures    earthquake    seismic    experimental    interdisciplinary    compressive    quantify    carbonates    progress    tests    guarantee    grenoble    observations    hazards    geo    university    scientific    dissipated    secondment    strategy    active    hosted    microstructural    remaining    off    newly    origin    economic    successful    damage    tensile    core    sinks    independent    terminate    wealth    earth    characterization    innovative    exhumed    release    striking    structural    seismicity    demonstrated    petrophysical    coseismic    vicinity    friction    world    scaling    researcher    overlooked    zones    carbonate    mechanisms    waves    relations    performed    natural    experiments    vast    amount    seismogenic    societal    combining    catastrophic    energy    nucleate    earthquakes    supervisors    extensive    mechanical    causing    heat    surface    generation    structure    systematically    loading    arguments    grow    tackles    destructive    dynamic    deadliest    strain    generally    universit    physical    theoretical    geophysical    multiscale    seismological    fault    rocks    whereas    manchester    huge   

Project "DAMAGE" data sheet

The following table provides information about the project.

Coordinator
UNIVERSITE GRENOBLE ALPES 

There are not information about this coordinator. Please contact Fabio for more information, thanks.

 Coordinator Country France [FR]
 Total cost 184˙707 €
 EC max contribution 184˙707 € (100%)
 Programme 1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
 Code Call H2020-MSCA-IF-2018
 Funding Scheme MSCA-IF-EF-ST
 Starting year 2020
 Duration (year-month-day) from 2020-01-13   to  2022-01-12

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    UNIVERSITE GRENOBLE ALPES FR (GRENOBLE) coordinator 184˙707.00
2    UNIVERSITE GRENOBLE ALPES FR (SAINT MARTIN D'HERES) coordinator 0.00

Map

 Project objective

Earthquakes are one of the deadliest geo-hazards in the world causing huge societal and economic impact. Destructive earthquakes are generally represented by ruptures which nucleate, grow and terminate along pre-existing faults with catastrophic strain energy release. Seismological observations and theoretical arguments demonstrated that most of earthquake energy is dissipated into heat by friction within the core of faults at depth. The remaining energy amount is the one driven to the Earth surface by seismic waves and associated to the generation of extensive DAMAGE in the vicinity of seismic faults. Vast research was recently performed to investigate on-fault mechanisms during earthquakes whereas much less has been done to constrain the physical processes and energy sinks associated to coseismic off-fault deformation. I propose here to systematically study off-fault coseismic damage in carbonates, which are the rocks where most of the destructive seismicity striking Europe is hosted. The proposed research is innovative since it tackles a scientific topic which was so far overlooked with a multiscale interdisciplinary approach combining: detailed field structural and geophysical characterization of exhumed active fault zones, compressive and tensile dynamic loading tests on carbonate rocks, and microstructural-petrophysical characterization of natural and experimental fault rocks. This integrated strategy will lead to build a wealth of novel datasets to quantify the damage structure and scaling relations of seismogenic fault zones in carbonates. Newly conceived rock deformation experiments will then help to determine the mechanical origin of coseismic damage in carbonates. The research will be conducted at Universitè Grenoble-Alpes with a secondment at University of Manchester. The experience of the supervisors and the equipment at both organizations will guarantee the successful progress of the research and my professional growth as independent researcher.

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The information about "DAMAGE" are provided by the European Opendata Portal: CORDIS opendata.

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