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RIFT-O-MAT SIGNED

Magma-Assisted Tectonics: two-phase dynamics of oceanic and continental rifts

Total Cost €

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EC-Contrib. €

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Partnership

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 RIFT-O-MAT project word cloud

Explore the words cloud of the RIFT-O-MAT project. It provides you a very rough idea of what is the project "RIFT-O-MAT" about.

incorporate    juan    observation    lithosphere    faults    viscoelastic    there    fuca    flow    tectonics    variation    solid    integral    distinguished    force    east    recognition    constraints    models    interact    phenomena    breaks    intrusion    continental    unresolved    rifts    mechanical    magmatic    rifting    tensile    chemical    functioning    mid    stress    consistent    relief    modest    assisted    outreach    indicates    deformation    plastic    source    geochemistry    theory    mathematics    weaken    code    strength    transform    suggests    plate    magma    inherent    governed    thermal    dynamics    understand    african    crustal    recorded    tectonic    sufficiently    dikes    innately    emplacement    supply    momentum    rock    rift    plates    consistently    crust    seismic    central    decades    tomography    continua    rheology    boundaries    mass    ocean    continents    lithospheric    africa    interpenetrating    ridge    validated    surface    lacking    almost    magmatism    hence    careful    excluded    de    frictional    faulting    basic    context    lavas    bathymetric    single    energy    divergent    diverse    fundamental    liquid    ground    modelled    ridges    thorough    conservation   

Project "RIFT-O-MAT" data sheet

The following table provides information about the project.

Coordinator
THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF OXFORD 

Organization address
address: WELLINGTON SQUARE UNIVERSITY OFFICES
city: OXFORD
postcode: OX1 2JD
website: www.ox.ac.uk

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 United Kingdom [UK]
 Total cost 2˙000˙000 €
 EC max contribution 2˙000˙000 € (100%)
 Programme 1. H2020-EU.1.1. (EXCELLENT SCIENCE - European Research Council (ERC))
 Code Call ERC-2017-COG
 Funding Scheme ERC-COG
 Starting year 2019
 Duration (year-month-day) from 2019-03-01   to  2024-02-29

 Partnership

Take a look of project's partnership.

# participants  country  role  EC contrib. [€] 
1    THE CHANCELLOR, MASTERS AND SCHOLARS OF THE UNIVERSITY OF OXFORD UK (OXFORD) coordinator 2˙000˙000.00

Map

 Project objective

There is widespread recognition of the central role of magma at divergent plate boundaries. However in almost all models, magmatism is treated as a by-product and is excluded from the dynamics. A thorough understanding of continental rifts and mid-ocean ridges, which are fundamental to plate tectonics, requires consistent models of magma intrusion into the lithosphere and crust. This is a proposal to develop models in which magmatism is an integral thermal, chemical, and mechanical component, and hence to better understand the basic functioning of plate tectonics.

Diverse insight and constraints on divergent boundaries come from decades of careful observation. But lacking adequate models of magmatism, old and new issues remain unresolved. For continents, a comparison of available tectonic force to inherent lithospheric strength indicates that magmatic intrusion is required to weaken plates sufficiently for rifting. For mid-ocean ridges, bathymetric analysis suggests that modest variation in the magma supply may be recorded by crustal emplacement and faulting. These phenomena cannot be understood and modelled in the context of single-phase flow. The proposed work breaks new ground in applying a theory that is innately two-phase; one where interpenetrating liquid and solid continua are governed by conservation of mass, momentum, and energy.

This theory will incorporate a viscoelastic-plastic/frictional rheology, modelling rock failure under tensile effective stress. Hence it will allow for dikes that interact consistently with faults. The open-source code will be validated by comparison with measurements of surface deformation/relief, products of seismic tomography, and geochemistry of lavas. In collaboration with distinguished project partners, models will be tailored to investigate the East African Rift System and Juan de Fuca ridge. Outreach will support mathematics in Africa. The proposed research will transform our understanding of magma-assisted tectonics.

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The information about "RIFT-O-MAT" are provided by the European Opendata Portal: CORDIS opendata.

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