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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.

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

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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