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PRESEISMIC SIGNED

Exploring the nucleation of large earthquakes: cascading and unpredictable or slowly driven and forecastable

Total Cost €

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EC-Contrib. €

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Partnership

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 PRESEISMIC project word cloud

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

observations    fault    mechanics    answering    mechanisms    attempts    extensive    usually    views    mainshock    slip    onset    predict    question    random    cascade    how    chile    estimation    slips    seismic    active    combining    nucleation    models    slow    assimilating    foreshocks    relationship    dynamic    unpredictable    first    procedure    catastrophic    ground    rapid    near    assimilation    capture    japan    types    entirely    cascades    triggered    probabilistic    preceded    relative    multiple    begin    opportunity    doomed    observe    algorithm    detector    independently    missing    data    unprecedented    slowly    events    aseismic    automated    monitor    tool    understand    motion    proportion    global    rupture    megathrust    failures    contrasting    contribution    faults    unified    forecast    genesis    datasets    cluttering    validation    quantitative    versus    physical    initiation    tsunami    accelerating    monitoring    explosion    dependent    estimates    continuous    earthquakes    deformation    belong    time    geodetic   

Project "PRESEISMIC" data sheet

The following table provides information about the project.

Coordinator
CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS 

Organization address
address: RUE MICHEL ANGE 3
city: PARIS
postcode: 75794
website: www.cnrs.fr

contact info
title: n.a.
name: n.a.
surname: n.a.
function: n.a.
email: n.a.
telephone: n.a.
fax: n.a.

 Coordinator Country France [FR]
 Total cost 1˙499˙545 €
 EC max contribution 1˙499˙545 € (100%)
 Programme 1. H2020-EU.1.1. (EXCELLENT SCIENCE - European Research Council (ERC))
 Code Call ERC-2018-STG
 Funding Scheme ERC-STG
 Starting year 2019
 Duration (year-month-day) from 2019-01-01   to  2023-12-31

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    CENTRE NATIONAL DE LA RECHERCHE SCIENTIFIQUE CNRS FR (PARIS) coordinator 1˙499˙545.00

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 Project objective

How do earthquakes begin? Answering this question is essential to understand fault mechanics but also to determine our ability to forecast large earthquakes. Although it is well established that some events are preceded by foreshocks, contrasting views have been proposed on the nucleation of earthquakes. Do these foreshocks belong to a cascade of random failures leading to the mainshock? Are they triggered by an aseismic nucleation phase in which the fault slips slowly before accelerating to a dynamic, catastrophic rupture? Will we ever be able to monitor and predict the slow onset of earthquakes or are we doomed to observe random, unpredictable cascades of events? We are currently missing a robust tool for quantitative estimation of the proportion of seismic versus aseismic slip during the rupture initiation, cluttering our attempts at understanding what physical mechanisms control the relationship between foreshocks and the onset of large earthquakes.

The current explosion of available near-fault ground-motion observations is an unprecedented opportunity to capture the genesis of earthquakes along active faults. I will develop an entirely new method based a novel data assimilation procedure that will produce probabilistic time-dependent slip models assimilating geodetic, seismic and tsunami datasets. While slow and rapid fault processes are usually studied independently, this unified approach will address the relative contribution of seismic and aseismic deformation.

The first step is the development of a novel probabilistic data assimilation method providing reliable uncertainty estimates and combining multiple data types. The second step is a validation of the method and an application to investigate the onset of recent megathrust earthquakes in Chile and Japan. The third step is the extensive, global use of the algorithm to the continuous monitoring of time-dependent slip along active faults providing an automated detector of the nucleation of earthquakes.

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

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