Opendata, web and dolomites

RIFT-O-MAT SIGNED

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

Total Cost €

0

EC-Contrib. €

0

Partnership

0

Views

0

 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.

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

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.

Are you the coordinator (or a participant) of this project? Plaese send me more information about the "RIFT-O-MAT" project.

For instance: the website url (it has not provided by EU-opendata yet), the logo, a more detailed description of the project (in plain text as a rtf file or a word file), some pictures (as picture files, not embedded into any word file), twitter account, linkedin page, etc.

Send me an  email (fabio@fabiodisconzi.com) and I put them in your project's page as son as possible.

Thanks. And then put a link of this page into your project's website.

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

More projects from the same programme (H2020-EU.1.1.)

CHIPTRANSFORM (2018)

On-chip optical communication with transformation optics

Read More  

CohoSing (2019)

Cohomology and Singularities

Read More  

SHExtreme (2020)

Estimating contribution of sub-hourly sea level oscillations to overall sea level extremes in changing climate

Read More