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.

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

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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