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.

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

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.)

ModGravTrial (2019)

Modified Gravity on Trial

Read More  

MuFLOART (2018)

Microbiological fluorescence observatory for antibiotic resistance tracking

Read More  

UEMHP (2019)

Unravelling Earth’s magnetic history and processes

Read More